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China Geology is delighted to announce the recipients of the Best Paper Awards, Highly Cited Paper Awards, Outstanding Editor Awards, and Outstanding Reviewer Awards for the year 2023. These awards aim to recognize papers of exceptional quality and impact, promote the scientific accomplishments of geological surveys, and acknowledge editorial board members and reviewers who provide outstanding support to the journal’s continuous development.

The Best Paper and Highly Cited Papers were meticulously selected from articles published in China Geology during 2022. The Best Paper were chosen for their academic quality and high impact in terms of citations and downloads (Sources: China Geology website, Web of Science and ScienceDirect). The Highly Cited Papers were selected based on the number of citations they received in 2023 as recorded in the Web of Science database, indicating the influence and recognition these papers garner in the field of geosciences.

The criteria for identifying Outstanding Editors encompass a wide range of contributions vital to the journal’s development, including topic proposal, author invitation, and peer review. The Outstanding Reviewers were selected based on the excellent quality, high quantity, and timeliness of their review reports.

Based on recommendation of the editorial team, the award candidates were rigorously evaluated and shortlisted by the Award Committee. We extend our heartfelt congratulations to the following authors, editorial board members and reviewers on winning the awards!

 

2023 Best Papers of China Geology

Index

Title

Authors

Article Information (Issue, Page Numbers, DOI)

1

Distribution characteristics, exploration and development, geological theories research progress and exploration directions of shale gas in China

Shi-zhen Li, Zhi Zhou, Hai-kuan Nie, Lei-fu Zhang, Teng Song, Wei-bin Liu, Hao-han Li, Qiu-chen Xu, Si-yu Wei, Shu Tao

China Geology, 5(1):110–135

DOI: 10.31035/cg2021069

2

Effects and mechanism of igneous rock on selenium in the tropical soil-rice system in Hainan Province, South China

Xiu-jin Liu, Ke Yang, Fei Guo, Shi-qi Tang, Ying-han Liu, Li Zhang, Hang-xin Cheng, Fei Liu

China Geology, 5(1):1–11

DOI: 10.31035/cg2021038

3

Paleozoic tectonic evolution of the eastern Central Asian Orogenic Belt in NE China

Yong-fei Ma, Yong-jiang Liu, A.Yu. Peskov, Yan Wang, Wei-min Song, Yu-jin Zhang, Cheng Qian, Tong-jun Liu

China Geology, 5(4):555–578

DOI: 10.31035/cg2021079

4

Molecular simulation studies on natural gas hydrates nucleation and growth: A review

Zheng-cai Zhang, Neng-you Wu, Chang-ling Liu, Xi-luo Hao, Yong-chao Zhang, Kai Gao, Bo Peng, Chao Zheng, Wei Tang,

Guang-jun Guo

China Geology, 5(2):330–344

DOI: 10.31035/cg2022017

5

Change trend of natural gas hydrates in permafrost on the Qinghai-Xizang Plateau (1960-2050) under the background of global warming and their impacts on carbon emissions

Zhen-quan Lu, Chu-guo Wu, Neng-you Wu, Hai-long Lu, Ting Wang, Rui Xiao, Hui Liu, Xin-he Wu

China Geology, 5(3): 475–509

DOI: 10.31035/cg2022034

6

Distribution, characteristics, and research status of microplastics in the trunk stream and main lakes of the Yangtze River: A review

Fang-ting Wang, Ke Bao, Chang-sheng Huang, Rui-ping Liu, Wen-jing Han, Cheng-yun Yi, Long Li, Yun Zhou

China Geology, 5(1):171–184

DOI: 10.31035/cg2022002

7

The first power generation test of hot dry rock resources exploration and production demonstration project in the Gonghe Basin, Qinghai Province, China

Er-yong Zhang, Dong-guang Wen, Gui-ling Wang, Wei-de Yan, Wen-shi Wang, Cheng-ming Ye, Xu-feng Li, Huang Wang, Xian-chun Tang, Wei Weng, Kuan Li, Chong-yuan Zhang, Ming-xing Liang, Hong-bao Luo, Han-yue Hu, Wei Zhang, Sen-qi Zhang, Xian-peng Jin, Hai-dong Wu, Lin-you Zhang, Qing-da Feng, Jing-yu Xie, Dan Wang, Yun-chao He, Yue-wei Wang, Zu-bin Chen, Zheng-pu Cheng, Wei-feng Luo, Yi Yang, Hao Zhang, En-lai Zha, Yu-lie Gong, Yu Zheng, Chang-sheng Jiang, Sheng-sheng Zhang, Xue Niu, Hui Zhang, Li-sha Hu, Gui-lin Zhu, Wen-hao Xu, Zhao-xuan Niu, Li Yang

China Geology, 5(3): 372–382

DOI: 10.31035/cg2022038

8

Soil geochemical prospecting prediction method based on deep convolutional neural networks-Taking Daqiao Gold Deposit in Gansu Province, China as an example

Yong-sheng Li, Chong Peng, Xiang-jin Ran, Lin-Fu Xue, She-li Chai

China Geology, 5(1):71–83

DOI: 10.31035/cg2021044

9

Geology and mineralization of the Pulang supergiant porphyry copper deposit (5.11 Mt) in Shangri-la, Yunnan Province, China: A review

Wen-chang Li, Xiang-fei Zhang, Hai-jun Yu, Dong Tao, Xue-long Liu

China Geology, 5(4):662–695

DOI: 10.31035/cg2022060

10

Gold enrichment characteristics and exploration prospects in Zambia: Based on 1 : 1000000 geochemical mapping

Jun-ping Ren, Jie Wang, A-lei Gu, Li-bo Zuo, Hong-wei Sun, Kang-kang Xu, Fu-Qing He, Chipilauka Mukofu, Alphet Phaskani

Dokowe, Ezekiah Chikambwe

China Geology, 5(1):60–70

DOI: 10.31035/cg2021034



2023 Top 10 Most Highly Cited Papers of China Geology (based on data up to March 2024)

Index

Title

Authors

Article Information

(Issue, Page Numbers, DOI)

1

Distribution characteristics, exploration and development, geological theories research progress and exploration directions of shale gas in China

Shi-zhen Li, Zhi Zhou, Hai-kuan Nie, Lei-fu Zhang, Teng Song, Wei-bin Liu, Hao-han Li, Qiu-chen Xu, Si-yu Wei, Shu Tao

China Geology, 5(1):110–135

DOI: 10.31035/cg2021069

2

Characteristics and sources of microplastic pollution in the water and sediments of the Jinjiang River Basin, Fujian Province, China

Ya-ci Liu, Lin Wu, Guo-wei Shi, Sheng-wei Cao, Ya-song Li

China Geology, 5(3): 429–438

DOI: 10.31035/cg2022051

3

The first power generation test of hot dry rock resources exploration and production demonstration project in the Gonghe Basin, Qinghai Province, China

Er-yong Zhang, Dong-guang Wen, Gui-ling Wang, Wei-de Yan, Wen-shi Wang, Cheng-ming Ye, Xu-feng Li, Huang Wang, Xian-chun Tang, Wei Weng, Kuan Li, Chong-yuan Zhang, Ming-xing Liang, Hong-bao Luo, Han-yue Hu, Wei Zhang, Sen-qi Zhang, Xian-peng Jin, Hai-dong Wu, Lin-you Zhang, Qing-da Feng, Jing-yu Xie, Dan Wang, Yun-chao He, Yue-wei Wang, Zu-bin Chen, Zheng-pu Cheng, Wei-feng Luo, Yi Yang, Hao Zhang, En-lai Zha, Yu-lie Gong, Yu Zheng, Chang-sheng Jiang, Sheng-sheng Zhang, Xue Niu, Hui Zhang, Li-sha Hu, Gui-lin Zhu, Wen-hao Xu, Zhao-xuan Niu, Li Yang

China Geology, 5(3): 372–382

DOI: 10.31035/cg2022038

4

Current status and cause analysis of microplastic pollution in sea areas in China

Wei Xiong, Xi Mei, Bei-bei Mi, Hao Yang, Zong-zhu Han, Yong Zhang, Wen-chao Lü

China Geology, 5(1):160–170

DOI: 10.31035/cg2021072

5

Geological characteristics, metallogenic regularity, and research progress of lithium deposits in China

Bo Zhang, Fan-yu Qi, Xue-zheng Gao, Xiao-lei Li, Yun-tao Shang, Zhao-yu Kong, Li-qiong Jia, Jie Meng, Hui Guo, Fu-kang Fang,

Yan-bin Liu, Xiao Jiang, Hui Chai, Zi Liu, Xian-tao Ye, Guo-dong Wang

China Geology, 5(4):734–767

DOI: 10.31035/cg2022054

6

Effects and mechanism of igneous rock on selenium in the tropical soil-rice system in Hainan Province, South China

Xiu-jin Liu, Ke Yang, Fei Guo, Shi-qi Tang, Ying-han Liu, Li Zhang, Hang-xin Cheng, Fei Liu

China Geology, 5(1):1–11

DOI: 10.31035/cg2021038

7

Molecular simulation studies on natural gas hydrates nucleation and growth: A review

Zheng-cai Zhang, Neng-you Wu, Chang-ling Liu, Xi-luo Hao, Yong-chao Zhang, Kai Gao, Bo Peng, Chao Zheng, Wei Tang,

Guang-jun Guo

China Geology, 5(2):330–344

DOI: 10.31035/cg2022017

8

Paleozoic tectonic evolution of the eastern Central Asian Orogenic Belt in NE China

Yong-fei Ma, Yong-jiang Liu, A.Yu. Peskov, Yan Wang, Wei-min Song, Yu-jin Zhang, Cheng Qian, Tong-jun Liu

China Geology, 5(4):555–578

DOI: 10.31035/cg2021079

9

Distribution, characteristics, and research status of microplastics in the trunk stream and main lakes of the Yangtze River: A review

Fang-ting Wang, Ke Bao, Chang-sheng Huang, Rui-ping Liu, Wen-jing Han, Cheng-yun Yi, Long Li, Yun Zhou

China Geology, 5(1):171–184

DOI: 10.31035/cg2022002

10

Experimental study on characteristics of pore water conversion during methane hydrates formation in unsaturated sand

Yun-kai Ji, Chang-ling Liu, Zhun Zhang, Qing-guo Meng, Le-le Liu, Yong-chao Zhang, Neng-you Wu

China Geology, 5(2):276–284

DOI: 10.31035/cg2022013

 


2023 Outstanding Editors of China Geology

Index

Name

Institution

1

Yan-long Li

Qingdao Institute of Marine Geology, China Geological Survey

2

Nan-sheng Qiu

China University of Petroleum (Beijing)

3

Yong-shuang Zhang

China University of Geosciences (Beijing)

4

Xiu-gen Fu

Southwest Petroleum University

5

Si-yuan Ye

Qingdao Institute of Marine Geology, China Geological Survey

 

2023 Outstanding Reviewers of China Geology

Index

Name

Institution

1

Lei Chen

China University of Petroleum (Huadong)

2

Guo-heng Liu

China University of Petroleum (Huadong)

3

Jia-xi Zhou

Yunnan University

4

Yao-hua Li

Oil and Gas Survey, China Geological Survey

5

Chang-bao Guo

Institute of Geomechanics, Chinese Academy of Geological Sciences

6

Wen-geng Cao

Institute of Hydrogeology and Environmental Geology, CAGS

7

Bai-qiang Li

Northwest University

8

Hua-feng Sun

Cores and Samples Center of Natural Resources, China Geological Survey

9

Fan Yang

Lanzhou University

10

De-gao Zhai

China University of Geosciences (Beijing)

China Geology Editorial Office

为鼓励广大作者创作出更多高质量科技论文，进一步增强地质调查成果在学术界的广泛影响，同时激励编委与审稿专家积极参与期刊的建设和发展工作，《中国地质（英文）》（《China Geology》）编辑部组织开展了2023年度的评选活动，旨在表彰优秀论文、高被引论文、优秀编委以及优秀审稿人。

评选优秀论文的过程中，主要参考了2022年期刊发表的论文在同行中的引用次数和下载量（官网、Web of Science、ScienceDirect）。高被引论文的评选则基于2022年期刊发表的论文在2023年度内的被引频次（Web of Science数据库），一定程度反映了论文在地学界的影响力和认可度。优秀编委的评选重点关注了期刊编委会成员为期刊作出的突出贡献，包括参与选题、组稿、审稿等工作的表现。优秀审稿人的评选综合考虑了审稿质量、数量以及审稿的时效性。

本次评选活动经过编辑部的精心推荐、部门研讨会以及专家评审会的严格筛选，最终遴选出《中国地质（英文）》2023年度优秀论文、高被引论文、优秀编委和优秀审稿人名单。现将结果公布如下。

 


2023年度《中国地质(英文)》优秀论文名单

序号

论文题目

作者

发表信息【期刊名称，卷（期）:起止页码, DOI】

1

Distribution characteristics, exploration and development, geological theories research progress and exploration directions of shale gas in China

Shi-zhen Li, Zhi Zhou, Hai-kuan Nie, Lei-fu Zhang, Teng Song, Wei-bin Liu, Hao-han Li, Qiu-chen Xu, Si-yu Wei, Shu Tao

China Geology, 5(1):110–135

DOI: 10.31035/cg2021069

2

Effects and mechanism of igneous rock on selenium in the tropical soil-rice system in Hainan Province, South China

Xiu-jin Liu, Ke Yang, Fei Guo, Shi-qi Tang, Ying-han Liu, Li Zhang, Hang-xin Cheng, Fei Liu

China Geology, 5(1):1–11

DOI: 10.31035/cg2021038

3

Paleozoic tectonic evolution of the eastern Central Asian Orogenic Belt in NE China

Yong-fei Ma, Yong-jiang Liu, A.Yu. Peskov, Yan Wang, Wei-min Song, Yu-jin Zhang, Cheng Qian, Tong-jun Liu

China Geology, 5(4):555–578

DOI: 10.31035/cg2021079

4

Molecular simulation studies on natural gas hydrates nucleation and growth: A review

Zheng-cai Zhang, Neng-you Wu, Chang-ling Liu, Xi-luo Hao, Yong-chao Zhang, Kai Gao, Bo Peng, Chao Zheng, Wei Tang,

Guang-jun Guo

China Geology, 5(2):330–344

DOI: 10.31035/cg2022017

5

Change trend of natural gas hydrates in permafrost on the Qinghai-Xizang Plateau (1960-2050) under the background of global warming and their impacts on carbon emissions

Zhen-quan Lu, Chu-guo Wu, Neng-you Wu, Hai-long Lu, Ting Wang, Rui Xiao, Hui Liu, Xin-he Wu

China Geology, 5(3): 475–509

DOI: 10.31035/cg2022034

6

Distribution, characteristics, and research status of microplastics in the trunk stream and main lakes of the Yangtze River: A review

Fang-ting Wang, Ke Bao, Chang-sheng Huang, Rui-ping Liu, Wen-jing Han, Cheng-yun Yi, Long Li, Yun Zhou

China Geology, 5(1):171–184

DOI: 10.31035/cg2022002

7

The first power generation test of hot dry rock resources exploration and production demonstration project in the Gonghe Basin, Qinghai Province, China

Er-yong Zhang, Dong-guang Wen, Gui-ling Wang, Wei-de Yan, Wen-shi Wang, Cheng-ming Ye, Xu-feng Li, Huang Wang, Xian-

chun Tang, Wei Weng, Kuan Li, Chong-yuan Zhang, Ming-xing Liang, Hong-bao Luo, Han-yue Hu, Wei Zhang, Sen-qi Zhang, Xian-peng Jin, Hai-dong Wu, Lin-you Zhang, Qing-da Feng, Jing-yu Xie, Dan Wang, Yun-chao He, Yue-wei Wang, Zu-bin Chen, Zheng-pu Cheng, Wei-feng Luo, Yi Yang, Hao Zhang, En-lai Zha, Yu-lie Gong, Yu Zheng, Chang-sheng Jiang, Sheng-sheng

Zhang, Xue Niu, Hui Zhang, Li-sha Hu, Gui-lin Zhu, Wen-hao Xu, Zhao-xuan Niu, Li Yang

China Geology, 5(3): 372–382

DOI: 10.31035/cg2022038

8

Soil geochemical prospecting prediction method based on deep convolutional neural networks-Taking Daqiao Gold Deposit in Gansu Province, China as an example

Yong-sheng Li, Chong Peng, Xiang-jin Ran, Lin-Fu Xue, She-li Chai

China Geology, 5(1):71–83

DOI: 10.31035/cg2021044

9

Geology and mineralization of the Pulang supergiant porphyry copper deposit (5.11 Mt) in Shangri-la, Yunnan Province, China: A review

Wen-chang Li, Xiang-fei Zhang, Hai-jun Yu, Dong Tao, Xue-long Liu

China Geology, 5(4):662–695

DOI: 10.31035/cg2022060

10

Gold enrichment characteristics and exploration prospects in Zambia: Based on 1 : 1000000 geochemical mapping

Jun-ping Ren, Jie Wang, A-lei Gu, Li-bo Zuo, Hong-wei Sun, Kang-kang Xu, Fu-Qing He, Chipilauka Mukofu, Alphet Phaskani

Dokowe, Ezekiah Chikambwe

China Geology, 5(1):60–70

DOI: 10.31035/cg2021034

 

2023年度《中国地质(英文)》十大高被引论文名单（截至2024年3月）

序号

论文题目

作者

发表信息【期刊名称，卷（期）:起止页码, DOI】

 

1

Distribution characteristics, exploration and development, geological theories research progress and exploration directions of shale gas in China

Shi-zhen Li, Zhi Zhou, Hai-kuan Nie, Lei-fu Zhang, Teng Song, Wei-bin Liu, Hao-han Li, Qiu-chen Xu, Si-yu Wei, Shu Tao

China Geology, 5(1):110–135

DOI: 10.31035/cg2021069

2

Characteristics and sources of microplastic pollution in the water and sediments of the Jinjiang River Basin, Fujian Province, China

Ya-ci Liu, Lin Wu, Guo-wei Shi, Sheng-wei Cao, Ya-song Li

China Geology, 5(3): 429–438

DOI: 10.31035/cg2022051

3

The first power generation test of hot dry rock resources exploration and production demonstration project in the Gonghe Basin, Qinghai Province, China

Er-yong Zhang, Dong-guang Wen, Gui-ling Wang, Wei-de Yan, Wen-shi Wang, Cheng-ming Ye, Xu-feng Li, Huang Wang, Xian-chun Tang, Wei Weng, Kuan Li, Chong-yuan Zhang, Ming-xing Liang, Hong-bao Luo, Han-yue Hu, Wei Zhang, Sen-qi Zhang, Xian-peng Jin, Hai-dong Wu, Lin-you Zhang, Qing-da Feng, Jing-yu Xie, Dan Wang, Yun-chao He, Yue-wei Wang, Zu-bin Chen, Zheng-pu Cheng, Wei-feng Luo, Yi Yang, Hao Zhang, En-lai Zha, Yu-lie Gong, Yu Zheng, Chang-sheng Jiang, Sheng-sheng Zhang, Xue Niu, Hui Zhang, Li-sha Hu, Gui-lin Zhu, Wen-hao Xu, Zhao-xuan Niu, Li Yang

China Geology, 5(3): 372–382

DOI: 10.31035/cg2022038

4

Current status and cause analysis of microplastic pollution in sea areas in China

Wei Xiong, Xi Mei, Bei-bei Mi, Hao Yang, Zong-zhu Han, Yong Zhang, Wen-chao Lü

China Geology, 5(1):160–170

DOI: 10.31035/cg2021072

5

Geological characteristics, metallogenic regularity, and research progress of lithium deposits in China

Bo Zhang, Fan-yu Qi, Xue-zheng Gao, Xiao-lei Li, Yun-tao Shang, Zhao-yu Kong, Li-qiong Jia, Jie Meng, Hui Guo, Fu-kang Fang,

Yan-bin Liu, Xiao Jiang, Hui Chai, Zi Liu, Xian-tao Ye, Guo-dong Wang

China Geology, 5(4):734–767

DOI: 10.31035/cg2018044

6

Effects and mechanism of igneous rock on selenium in the tropical soil-rice system in Hainan Province, South China

Xiu-jin Liu, Ke Yang, Fei Guo, Shi-qi Tang, Ying-han Liu, Li Zhang, Hang-xin Cheng, Fei Liu

China Geology, 5(1):1–11

DOI: 10.31035/cg2021038

7

Molecular simulation studies on natural gas hydrates nucleation and growth: A review

Zheng-cai Zhang, Neng-you Wu, Chang-ling Liu, Xi-luo Hao, Yong-chao Zhang, Kai Gao, Bo Peng, Chao Zheng, Wei Tang,

Guang-jun Guo

China Geology, 5(2):330–344

DOI: 10.31035/cg2022017

8

Paleozoic tectonic evolution of the eastern Central Asian Orogenic Belt in NE China

Yong-fei Ma, Yong-jiang Liu, A.Yu. Peskov, Yan Wang, Wei-min Song, Yu-jin Zhang, Cheng Qian, Tong-jun Liu

China Geology, 5(4):555–578

DOI: 10.31035/cg2021079

9

Distribution, characteristics, and research status of microplastics in the trunk stream and main lakes of the Yangtze River: A review

Fang-ting Wang, Ke Bao, Chang-sheng Huang, Rui-ping Liu, Wen-jing Han, Cheng-yun Yi, Long Li, Yun Zhou

China Geology, 5(1):171–184

DOI: 10.31035/cg2022002

10

Experimental study on characteristics of pore water conversion during methane hydrates formation in unsaturated sand

Yun-kai Ji, Chang-ling Liu, Zhun Zhang, Qing-guo Meng, Le-le Liu, Yong-chao Zhang, Neng-you Wu

China Geology, 5(2):276–284

DOI: 10.31035/cg2022013

 

2023年度《中国地质（英文）》优秀编委名单

序号

姓名

单位

1

李彦龙

中国地质调查局青岛海洋地质研究所

2

邱楠生

中国石油大学（北京）

3

张永双

中国地质大学（北京）

4

付修根

西南石油大学

5

叶思源

中国地质调查局青岛海洋地质研究所

 

2023年度《中国地质（英文）》优秀审稿人名单

序号

姓名

单位

1

陈  磊

中国石油大学（华东）

2

刘国恒

中国石油大学（华东）

3

周家喜

云南大学

4

李耀华

中国地质调查局油气资源调查中心

5

郭长宝

中国地质科学院地质力学研究所

6

曹文庚

中国地质科学院水文地质环境地质研究所

7

李百强

西北大学

8

孙华峰

中国地质调查局自然资源实物地质资料中心

9

杨  帆

兰州大学

10

翟德高

中国地质大学（北京）

 《中国地质（英文）》编辑部


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2023年度China Geology（《中国地质（英文）》）优秀论文、高被引论文、优秀编委、优秀审稿人评选结果","titleEn":"","type":""},"dataId":"115","dataType":"News","id":"eb8da52a-2a52-4c50-9197-6eb9a4d438bb","language":"en","sort":1,"tagId":"0"},{"data":{"browseNum":553,"content":"

The SinoProbe Center of the China Geological Survey is a geosciences innovation center for deep geological surveys and deep process researches, which is also the national base for deep exploration and deep earth science researches in China. The center is mainly focused on deep explorations of the earth, deep geological surveys and fundamental researches on deep earth science. The main missions of the SinoProbe Center are to undertake research programs on deep earth structural and compositional exploration, technology research and development on deep earth exploration, exploitation and evaluation of deep oil and gas, deep mineral resources, deep geothermal energy, and underground space exploration and utilization.


 1. Organization and leading experts

Honorary directors: Ting-dong Li (member of CAS), Yuchuan Chen (member of CAS) 

Director: Guang-sheng Yan (research professor) Deputy directors: Qing-tian Lü (research professor), Yan Ma (research professor)

Leading scientists: Shu-wen Dong (research professor), Ri-xiang Zhu (member of CAS), Cheng-shan Wang (member of CAS), Rui Gao (member of CAS), Zeng-qian Hou (member of CAS), Zong-li Huang (research professor), Da Wang (Research Professor), De-wu Qiao (Research Professor).

2. Divisions of the SinoProbe Center

2.1. Division of crustal structure and deep energy exploration and evaluation

This division is based on geophysical technologies, multidisciplinary and multi-deep exploration scales to reveal the deep processes, 3D structures, and metallogenic processing of the typical metallogenic belts or ore-concentrated areas in the deep earth. The division is aimed to construct regional metallogenic dynamics, discover innovative technologies and methods of geophysical data collection, processing,develop multi-databased inversion and lithological recognition methods,and set up technical combined system of deep mineral deposits exploration.

2.2. Division of crustal structure and deep energy exploration and evaluation

This division is focused on deep and ultra-deep structure exploration of oil and gas potentials, evaluation of largescaled orogenic petroliferous basin belts, and new oil and gas strata discoveries in the North China basins to further explore deep oil and gas resources.

2.3. Division of underground space exploration and utilization

This division is aimed to carry out following technologies such as anti-interference high precision geophysical techniques, underground drilling and logging techniques with precise localization and monitoring techniques, multiple parameter information integration and AI modeling, collaborative planning and utilization of underground and ground spaces, dynamic information system of construction, utilization of underground caves and fractures, construction of underground self-circulation ecosystem, and monitoring evaluation system of underground space engineering.

2.4. Division of geothermal energy and groundwater research

This division is concentrated on modeling evolution history of the tectonic controlled geothermal system studies, geophysical explorations, high temperature drilling and geothermal logging studies, and reservoir environments and re-injection technologies developments.

2.5. Division of ultra-deep scientific drilling

This division is focused on general design and operation management of ultra-deep scientific drilling programs, developing ultra-deep drilling equipments, drilling technologies and materials, constructions of simulation laboratory for high P–T drilling and analysis center for drilling samples, and implementing scientific drilling programs for major geological problems in key areas.

2.6. Division of deep earth science

This division is aimed to reveal the 3D structure, deep processes, and deep earth geodynamics of the continental lithosphere through structural and compositional explorations.Geophysical seismic profiling will be used to study tectonic boundaries and basement.The deep earth science division will use physical simulation of geological structures to study deformation mechanism and theories. Moreover, to carry out deep structural exploration and integration research on the uplift and growth, geodynamic evolution of the Xizang plateau, and its resource and environmental effects, the division will be highly concentrated on studying the Xizang plateau and surrounding basin-range junction belts.

2.7. Division of data management and sharing

This division manages the submission, collection,integration, releasing and public sharing of the national big data on deep exploration, 3D geodynamic modeling of the continental lithosphere,and 3D visualization of the deep earth.

2.8. Division of large equipment operation and maintenance

This division is responsible for large equipment configuration, deployment, and regular maintenance. It will also provide standardization and coordination services of the equipments, sharing service to outside institutions. The division is in charge of executing the technical upgrade, renovation, and independent development of the deep exploration equipment. Annual equipment procurement plan and operating status report will be published from the large equipment division.

2.9. Division of administration

The administration division is responsible for daily management, international cooperation, and public service.

3. Technical equipments

3.1. Deep structure detection system

The center is equipped with the Qiandao seismograph system, broadband seismograph, magnetotelluric instrument, large-scale parallel computing system, data center, and realtime monitoring system.

3.2. Deep material composition and analysis system

The center has 16 scanning electron microscopes, including one ion probe, two electron probes, one transmission electron microscope, three rock core scanners, four laser Raman spectrometers and five X-ray diffractometers (XRD), which are mainly used for testing morphology, phase and microstructure of rock minerals.

3.3. High temperature and high pressure experimental simulation system

The center has more than 10 experimental equipments on rock mechanics, high temperature and high pressure experiments etc., which can be used to test drilling fluid flow characteristics, rock shear fracture friction heat, low permeability rock properties in high temperature and high pressure conditions.

4. International exchanges and cooperation

Being in close collaboration with the International Union of Geological Sciences (IUGS), the International Continental Scientific Drilling Program (ICSD), the International Lithosphere Program etc., and the center is ambitious to launch large international science projects on deep exploration and to lead an international organization of urban geology and underground space. The SinoProbe Center plans to hold abundant internationally conferences on deep exploration to improve international cooperation in the future.

5. Contact

The SinoProbe Center, CAGS
Address: No. 26 Baiwanzhuang Road, Xicheng District,
Beijing 100037, China
Tel: +86-(10)-68999360 Fax: +86-(10)-68310894
http://www.sinoprobe.org

","downloadFile":"0","id":75,"imagePath":"","linkedWebsite":"","newsColumn":{"abbreviation":"news","breviaryShowNum":10,"columnNewsTemplate":"news_detail_en.vm","createTime":"2017-06-26 00:00:00","id":11,"journalId":"ff007540-a7c7-4752-b593-efa08309babb","language":"en","level":2,"mobileShow":1,"name":"News","oldId":"c3ca57d7-2bb4-47d5-a460-9d96d18f7671","openTarget":"_top","parent":{"abbreviation":"newsanddata","columnNewsTemplate":"news_detail_en.vm","createTime":"2017-12-29 00:00:00","id":17,"journalId":"ff007540-a7c7-4752-b593-efa08309babb","language":"en","level":1,"mobileShow":1,"name":"News & Data","oldId":"13712de2-f738-4442-8f43-73a3f9e1c68c","openTarget":"_top","showLocation":"1","sort":4,"state":"1","type":"1","updateTime":"2022-06-30 00:00:00","urlLink":"javascript:void(0);","urlLinkAPP":"javascript:void(0);"},"showLocation":"1","sort":2,"state":"1","type":"1","updateTime":"2018-06-06 00:00:00","urlLink":"","urlLinkAPP":""},"openTarget":"_top","outputName":"","releaseState":"publish","releaseTime":"2018-05-22 10:59:36","releaseYear":"2018","tags":[{"data":"{\"publisherId\":\"\",\"journalName\":\"\",\"remark\":\"\",\"createDate\":\"\",\"createUser\":\"\",\"status\":\"1\"}","id":"0","journalId":"ff007540-a7c7-4752-b593-efa08309babb","level":1,"nameCn":"轮播推荐","nameEn":"轮播推荐","outputName":"0","sort":0,"tags":[],"type":"recommend"}],"title":"Introduction of the SinoProbe Center, China Geological Survey","titleEn":"","type":""},"dataId":"75","dataType":"News","id":"6e2a68b5-5fa2-4890-bd56-e90ef2c018c1","language":"en","sort":2,"tagId":"0"},{"data":{"abstractAccess":true,"abstractinfoCn":"","abstractinfoEn":"Frugivory is an important ecological tie between animals and angiosperms. It plays an important role in the evolution of food webs and energy flow networks in the ecosystem. However, little is known about how old this relationship can be due to lack of relevant fossil evidence. Here, the authors report a fossil fruit, Jurafructus gen. nov., a putative angiosperm from the Middle−Late Jurassic (>164 Ma) of Daohugou Village, Inner Mongolia, China, which provides the currently earliest evidence of frugivory. The fossil is a more or less three-dimensionally preserved coalified drupe that has been damaged by animals in two different ways. The pericarp, in addition to the seed coat surrounding parenchyma seed contents, is suggestive of an angiospermous affinity, as such a 3+3 structure is distinct from a three-layered seed coat in gymnosperms. The seed possesses a distal micropyle, attached on the base of the pericarp, suggestive of a former orthotropous ovule in the gynoecium. The damaged pericarp of Jurafructus suggests that frugivory can be dated back to the Middle−Late Jurassic. Apparently, the ecological relationship between angiosperms and animals extends deep into the fossil record.","appendixList":[],"articleBusiness":{"articleId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","articleState":"-1","articleType":"1","baiduIncludeResult":0,"baiduIncludeResultSearchNum":3,"baiduXueShuIncludeResult":0,"baiduXueShuIncludeResultSearchNum":0,"filename":"cg2020010.xml","googleIncludeResult":0,"googleIncludeResultSearchNum":0,"htmlSource":1,"htmlViewCount":441,"id":"a0083a4f-3188-44f7-9617-5f07e8a67d99","isRegCstr":0,"isRegDOI":0,"isUpdate":"1","pdfDownCount":101,"pdfEnFileSizeInt":0,"pdfFileName":"cg2020010.pdf","pdfFileSize":18812.54,"pdfFileSizeInt":18812,"remark":"XML","seoInfo":"","viewCount":4758,"xmlDownCount":0,"xmlFileSize":80.69},"articleNo":"cg2020010","authors":[{"addressTagIds":"aff1","articleId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","authorNameCn":"","authorNameEn":"Li-jun Chen","authorTagVal":"a","authorType":"author","corresper":false,"givenNamesEn":"Li-jun","id":"a958677c-cd66-4aa1-8a8b-d8362bd9ef9a","sortNumber":1,"surNameEn":"Chen"},{"addressTagIds":"aff2","articleId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","authorNameCn":"","authorNameEn":"Ye-mao Hou","authorTagVal":"b","authorType":"author","corresper":false,"givenNamesEn":"Ye-mao","id":"b757a1aa-6e74-427b-a568-785ed23d9f0e","sortNumber":2,"surNameEn":"Hou"},{"addressTagIds":"aff2","articleId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","authorNameCn":"","authorNameEn":"Peng-fei Yin","authorTagVal":"b","authorType":"author","corresper":false,"givenNamesEn":"Peng-fei","id":"fadcfa65-1c8e-482f-b192-52a41fb8d9f8","sortNumber":3,"surNameEn":"Yin"},{"addressTagIds":"aff3,aff4","articleId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","authorNameCn":"","authorNameEn":"Xin Wang","authorTagVal":"c,d","authorType":"author","corresper":true,"correspinfoEn":"xinwang@nigpas.ac.cn (Xin Wang)","email":"xinwang@nigpas.ac.cn","givenNamesEn":"Xin","id":"fd3bd60f-cbca-48e2-ab9b-d271da5efc9f","sortNumber":4,"surNameEn":"Wang"}],"categoryNameEn":"Original Articles","citationCn":"","citationEn":"Chen Li-jun, Hou Ye-mao, Yin Peng-fei, Wang Xin. 2020. An edible fruit from the Jurassic of China. China Geology, 3(1), 8‒15. doi: 10.31035/cg2020010.","doi":"10.31035/cg2020010","figList":[{"dataId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","fileFrom":"xml","fileLastName":"jpg","filePath":"/fileZGDZYW/journal/article/zgdzyw/2020/1/cg2020010-1.jpg","fileSize":"121KB","fileType":"fulltextFig","fileXMLPath":"cg2020010-1.jpg","id":"750ac034-074c-42b5-8e4f-2af1485806b3","journalId":"ff007540-a7c7-4752-b593-efa08309babb","labelText":"1","nameEn":"Geographical information of the fossil locality of Jurafructus gen. nov., Daohugou Village, Inner Mongolia, China (b). The inset map (a) shows northeastern China, and the rectangular region is enlarged in (b). The main map (b) shows the junction region among Liaoning Province, Hebei Province and Inner Mongolia. The arrow points to the fossil locality of Daohugou Village.","referSecTagIds":"","sort":0,"supplementRemarkCn":"","supplementRemarkEn":"","tagId":"Figure1","type":"article","typesetSecTagId":"s02","viewNum":0},{"dataId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","fileFrom":"xml","fileLastName":"jpg","filePath":"/fileZGDZYW/journal/article/zgdzyw/2020/1/cg2020010-2.jpg","fileType":"fulltextFig","fileXMLPath":"cg2020010-2.jpg","id":"c7aeea55-cb9d-4011-ac3e-5162c47c8d60","journalId":"ff007540-a7c7-4752-b593-efa08309babb","labelText":"2","nameEn":"General view of Jurafructus. a−coalified more or less three-dimensionally preserved fruit; b−the same as in Fig. 2a, but using SEM. Note the attachment (between arrows) of seed (S) on the bottom of the urceolate pericarp (P). The rectangular regions are shown in detail in Fig. 3.","referSecTagIds":"","sort":1,"supplementRemarkCn":"","supplementRemarkEn":"","tagId":"Figure2","type":"article","typesetSecTagId":"s02","viewNum":0},{"dataId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","fileFrom":"xml","fileLastName":"jpg","filePath":"/fileZGDZYW/journal/article/zgdzyw/2020/1/cg2020010-4.jpg","fileSize":"2926KB","fileType":"fulltextFig","fileXMLPath":"cg2020010-4.jpg","id":"fd85a663-d4da-4c1f-a072-2a2f58e7c186","journalId":"ff007540-a7c7-4752-b593-efa08309babb","labelText":"4","nameEn":"Micro-CT renderings of Jurafructus. a−longitudinal planar view of the fruit, showing the seed (s) separated from the enclosing pericarp (p) at its top. Note the missing patchy portion of pericarp and/or seed coat; b−detailed view of the pericarp at the fruit tip; c−longitudinal view of the fruit tip, showing the pericarp (p) and micropyle (arrow) at the seed top; d−longitudinal section of the fruit tip, showing seed tip (s) sandwiched by the pericarp (p). Note the separation (arrow) between the pericarp and seed; e−f−two longitudinal views of the fruit showing the damaged surface (broken lines between arrows) in seed (s) and pericarp (p); g−longitudinal view of the fruit showing tissue residue (arrow) after damaging and the original surface (broken line); h−longitudinal view of the fruit, showing the distal appendages (arrow). Bottom of the fruit is to the left of the figure.","referSecTagIds":"","sort":2,"supplementRemarkCn":"","supplementRemarkEn":"","tagId":"Figure4","type":"article","typesetSecTagId":"s02","viewNum":0},{"dataId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","fileFrom":"xml","fileLastName":"jpg","filePath":"/fileZGDZYW/journal/article/zgdzyw/2020/1/cg2020010-5.jpg","fileSize":"1042KB","fileType":"fulltextFig","fileXMLPath":"cg2020010-5.jpg","id":"f9a37e8e-409e-4825-8b7f-3b70a8b68e03","journalId":"ff007540-a7c7-4752-b593-efa08309babb","labelText":"5","nameEn":"Diagram of Jurafructus showing a section through the center of the fruit. Not to scale. Note the appendages (1) at the apex and stalk at the base (11), three-layered pericarp (2, 3, 4) fully enclosing three layered seed coat (5, 6, 7), which surrounds the seed contents (8), piercing damage (9) and patchy damage (12) on the fruit surface. The seed is attached at the base (10) and has a micropyle at the top (13).","referSecTagIds":"","sort":3,"supplementRemarkCn":"","supplementRemarkEn":"","tagId":"Figure5","type":"article","typesetSecTagId":"s03","viewNum":0},{"dataId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","fileFrom":"xml","fileLastName":"jpg","filePath":"/fileZGDZYW/journal/article/zgdzyw/2020/1/cg2020010-3.jpg","fileType":"fulltextFig","fileXMLPath":"cg2020010-3.jpg","id":"9b13f904-6688-450c-9b6f-ac6d933514a8","journalId":"ff007540-a7c7-4752-b593-efa08309babb","labelText":"3","nameEn":"SEM views of Jurafructus. a−detailed view of the upper-right rectangle in Fig. 2b, showing the surface view of the seed coat (white line) and seed contents (SC) inside; b−detailed surface view of the seed coat, showing longitudinally oriented elongated cells, enlarged from the upper rectangle in Fig. 3a; c−detailed view of the seed coat, showing rugose surface texture, enlarged from the lower rectangle in Fig. 3a; d−detailed view of the lower-right rectangle in Fig. 2b, showing the seed contents (SC) and surrounding 3+3 organization (three-layered seed coat (S3, S2, S1) PLUS three-layered pericarp (P3, P2, P1)). Note that the P2 is not continuous but interrupted at the position corresponding to the depression on fruit surface (arrow); e−detailed view of seed coat with three layers (S1, S2, S3); f−detailed view of the left rectangle in Fig. 2b, showing the epidermis (ep), three-layered pericarp (P1, P2, P3); g−spongy subcellular details of the parenchymatous cells in the seed contents; h−texture on the sclerenchymatous cells in S2 layer of seed coat.","referSecTagIds":"","sort":4,"supplementRemarkCn":"","supplementRemarkEn":"","tagId":"Figure3","type":"article","typesetSecTagId":"s03","viewNum":0}],"filePath":"/fileZGDZYW/journal/article/zgdzyw/2020/1/","firstFig":{"dataId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","fileFrom":"xml","fileLastName":"jpg","filePath":"/fileZGDZYW/journal/article/zgdzyw/2020/1/cg2020010-1_mini.jpg","fileSize":"121KB","fileType":"fulltextFig","fileXMLPath":"cg2020010-1.jpg","id":"750ac034-074c-42b5-8e4f-2af1485806b3","journalId":"ff007540-a7c7-4752-b593-efa08309babb","labelText":"1","nameEn":"Geographical information of the fossil locality of Jurafructus gen. nov., Daohugou Village, Inner Mongolia, China (b). The inset map (a) shows northeastern China, and the rectangular region is enlarged in (b). The main map (b) shows the junction region among Liaoning Province, Hebei Province and Inner Mongolia. The arrow points to the fossil locality of Daohugou Village.","referSecTagIds":"","sort":0,"supplementRemarkCn":"","supplementRemarkEn":"","tagId":"Figure1","type":"article","typesetSecTagId":"s02","viewNum":0},"hasPage":true,"htmlAccess":true,"id":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","issue":"1","issueArticle":"0","keywords":[{"articleId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","id":"facc671c-0709-4bd7-bfc2-5e4df630eff8","keywordEn":"Jurafructus","sortNum":1},{"articleId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","id":"a82941fb-59f0-4d11-9067-d9b6ffead3df","keywordEn":"Jurassic","sortNum":2},{"articleId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","id":"8f1edd84-0be6-4ce8-93bd-d01798ed7c0d","keywordEn":"Angiosperm","sortNum":3},{"articleId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","id":"f8435e58-d5d6-4134-b043-536b00b9adb6","keywordEn":"Evolution","sortNum":4},{"articleId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","id":"8380d3a5-4cde-4315-ad54-bddcc42ca73c","keywordEn":"Animals","sortNum":5},{"articleId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","id":"646068ce-4c57-446b-b9d6-9d96e4490e79","keywordEn":"Frugivory","sortNum":6},{"articleId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","id":"dd7bec12-ebc9-4b01-a894-d5b06c946025","keywordEn":"Fruit","sortNum":7},{"articleId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","id":"d9f8f690-671a-4324-9b0b-060ef6caeaca","keywordEn":"China","sortNum":8}],"language":"en","notes":[],"page":"8-15","pdfAccess":true,"publisherId":"cg2020010","releaseProgress":{"articleId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","lastReleaseTime":"2020-12-23 11:45","maxLastReleaseTime":"2020-12-23 11:45","minLastReleaseTime":"2020-04-01 08:54","otherReleaseList":[{"articleId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","currentState":"Accepted Manuscript","currentStateEn":"Accepted Manuscript","lastReleaseTime":"2020-03-25 14:18","maxLastReleaseTime":"2020-03-25 14:18","minLastReleaseTime":"2020-03-18 19:11","otherReleaseList":[]}]},"releaseState":1,"searchSort":"20200001000000","subTitleCn":"","subTitleEn":"","supplements":[],"tableList":[],"tags":[{"data":"{\"publisherId\":\"\",\"journalName\":\"\",\"remark\":\"\",\"createDate\":\"\",\"createUser\":\"\",\"status\":\"1\"}","id":"0","journalId":"ff007540-a7c7-4752-b593-efa08309babb","level":1,"nameCn":"轮播推荐","nameEn":"轮播推荐","outputName":"0","sort":0,"tags":[],"type":"recommend"}],"titleCn":"","titleEn":"An edible fruit from the Jurassic of China","volume":"3","year":"2020","yearInt":2020},"dataId":"3bcf4412-f310-41e4-9d6a-a33f620ae54d","dataType":"Article","id":"3bcf4412-f310-41e4-9d6a-a33f620ae54d0","language":"en","sort":2,"tagId":"0"},{"data":{"abstractAccess":true,"abstractinfoCn":"","abstractinfoEn":"Regional aridity is increasing under global climate change, and therefore the sustainable use of water resources has drawn attention from scientists and the public. Land-use changes can have a significant impact on groundwater recharge in arid regions, and quantitative assessment of the impact is key to sustainable groundwater resources management. In this study, the changes of groundwater recharge after the conversion of natural lands to croplands were investigated and compared in inland and arid region, i.e., the northern slope of the Tianshan Mountain. Stable isotopes suggest that soil water in topsoil (< 2 m) has experienced stronger evaporation under natural lands than croplands, and then moves downward as a piston flow. Recharge was estimated by the tracer-based mass balance method, i.e., chloride and sulfate. Recharge rates under natural conditions estimated by the chloride mass balance (CMB) method were estimated to be 0.07 mm/a in deserts and 0.4 mm/a in oases. In contrast, the estimated groundwater recharge ranged from 61.2 mm/a to 44.8 mm/a in croplands, indicating that groundwater recharge would increase significantly after land changes from natural lands to irrigated croplands in arid regions. Recharge estimated by the sulfate mass balance method is consistent with that from the CMB method, indicating that sulfate is also a good tracer capable of estimating groundwater recharge.","appendixList":[],"articleBusiness":{"articleId":"0b4f03e1-ac58-45d5-9be4-cbbfd6d73d92","articleState":"-1","articleType":"1","baiduIncludeResult":0,"baiduIncludeResultSearchNum":3,"baiduXueShuIncludeResult":0,"baiduXueShuIncludeResultSearchNum":0,"filename":"cg2020008.xml","googleIncludeResult":0,"googleIncludeResultSearchNum":0,"htmlSource":1,"htmlViewCount":298,"id":"660fd750-d9c0-4365-a875-0bfbf775a041","isRegCstr":0,"isRegDOI":0,"isUpdate":"1","pdfDownCount":74,"pdfEnFileSizeInt":0,"pdfFileName":"cg2020008.pdf","pdfFileSize":16702.97,"pdfFileSizeInt":16702,"remark":"XML","viewCount":4161,"xmlDownCount":0,"xmlFileSize":172.06},"articleNo":"cg2020008","authors":[{"addressTagIds":"aff1","articleId":"0b4f03e1-ac58-45d5-9be4-cbbfd6d73d92","authorNameCn":"","authorNameEn":"Fang-qiang Sun","authorTagVal":"a","authorType":"author","corresper":false,"givenNamesEn":"Fang-qiang","id":"e4f057fe-1a33-4d59-96c7-f086424b4a17","sortNumber":1,"surNameEn":"Sun"},{"addressTagIds":"aff1","articleId":"0b4f03e1-ac58-45d5-9be4-cbbfd6d73d92","authorNameCn":"","authorNameEn":"Li-he Yin","authorTagVal":"a","authorType":"author","corresper":true,"correspinfoEn":"ylihe@cgs.cn (Li-he Yin)","email":"ylihe@cgs.cn","givenNamesEn":"Li-he","id":"8069c9d0-295d-42e7-ba3b-30a68d420706","sortNumber":2,"surNameEn":"Yin"},{"addressTagIds":"aff2","articleId":"0b4f03e1-ac58-45d5-9be4-cbbfd6d73d92","authorNameCn":"","authorNameEn":"Wu-hui Jia","authorTagVal":"b","authorType":"author","corresper":false,"givenNamesEn":"Wu-hui","id":"de5250c0-3963-44c3-aa88-3affe5ed8844","sortNumber":3,"surNameEn":"Jia"},{"addressTagIds":"aff1","articleId":"0b4f03e1-ac58-45d5-9be4-cbbfd6d73d92","authorNameCn":"","authorNameEn":"Jun Zhang","authorTagVal":"a","authorType":"author","corresper":false,"givenNamesEn":"Jun","id":"eef74e5a-119a-4641-8d6d-00940c35e9de","sortNumber":4,"surNameEn":"Zhang"},{"addressTagIds":"aff1","articleId":"0b4f03e1-ac58-45d5-9be4-cbbfd6d73d92","authorNameCn":"","authorNameEn":"Xiao-yong Wang","authorTagVal":"a","authorType":"author","corresper":false,"givenNamesEn":"Xiao-yong","id":"461b0dc9-4b0d-4ed0-8d20-34f90397bc60","sortNumber":5,"surNameEn":"Wang"},{"addressTagIds":"aff1","articleId":"0b4f03e1-ac58-45d5-9be4-cbbfd6d73d92","authorNameCn":"","authorNameEn":"Li-feng Zhu","authorTagVal":"a","authorType":"author","corresper":false,"givenNamesEn":"Li-feng","id":"e6b35321-8f5c-426f-9cb0-cb6ecd13deb0","sortNumber":6,"surNameEn":"Zhu"},{"addressTagIds":"aff3","articleId":"0b4f03e1-ac58-45d5-9be4-cbbfd6d73d92","authorNameCn":"","authorNameEn":"Xin-xin Zhang","authorTagVal":"c","authorType":"author","corresper":false,"givenNamesEn":"Xin-xin","id":"d4f30aac-e466-4f27-b86b-ab844d7b48b3","sortNumber":7,"surNameEn":"Zhang"},{"addressTagIds":"aff1","articleId":"0b4f03e1-ac58-45d5-9be4-cbbfd6d73d92","authorNameCn":"","authorNameEn":"Xiao-ping Tang","authorTagVal":"a","authorType":"author","corresper":false,"givenNamesEn":"Xiao-ping","id":"a21d44ff-301f-49b7-b0d2-e4f96136050f","sortNumber":8,"surNameEn":"Tang"},{"addressTagIds":"aff1","articleId":"0b4f03e1-ac58-45d5-9be4-cbbfd6d73d92","authorNameCn":"","authorNameEn":"Jia-qiu Dong","authorTagVal":"a","authorType":"author","corresper":false,"givenNamesEn":"Jia-qiu","id":"91373545-0495-4c26-aebc-d89ad5450fd6","sortNumber":9,"surNameEn":"Dong"}],"categoryNameEn":"Original Articles","citationCn":"","citationEn":"Sun Fang-qiang, Yin Li-he, Jia Wu-hui, Zhang Jun, Wang Xiao-yong, Zhu Li-feng, Zhang Xin-xin, Tang Xiao-ping, Dong Jia-qiu. 2020. 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Croplands vs. natural lands","volume":"3","year":"2020","yearInt":2020},"dataId":"0b4f03e1-ac58-45d5-9be4-cbbfd6d73d92","dataType":"Article","id":"0b4f03e1-ac58-45d5-9be4-cbbfd6d73d920","language":"en","sort":3,"tagId":"0"},{"data":{"browseNum":496,"content":"

\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t

Resource: Ministry of Natural Resources

China Mineral Resources 2015.pdf



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However, due to the dispute on the tectonic division of West Tianshan, the ore-controlling factors and the regional metallogenic laws are controversial. The authors analyze regional gravity data and notice that the high-value region corresponds to the Yili ancient continent, thus the southeastern boundary of the Yili ancient continent is delineated. Comparative analysis of gravity, aeromagnetic and geologic data reveals that the Tulasu basin, where some medium to large epithermal gold deposits locate, lies above the Yili ancient continent; the Yili Carboniferous-Permian rift extends in E-W direction, numbers of copper deposits have been found in the mid-west section of the rift which lies above the Yili ancient continent, whereas few copper deposits have been discovered in the east section which is outside the Yili ancient continent. Accordingly, the Yili ancient continent may be rich in gold, copper and other metal elements; the metal-bearing hydrothermal solution moves up with the activity of magmatism, and deposits in the favorable places (the Tulasu basin and the Yili Carboniferous-Permian rift), forming numerous small and medium gold, copper deposits, as well as some large and super-large gold deposits. Therefore, the tectonic-magmatic hydrothermal zone above the Yili ancient continent should be the prospective area for epithermal gold and copper polymetallic deposits.","appendixList":[],"articleBusiness":{"articleId":"8f885e29-71d0-4c75-88b5-b0fdf182d82a","articleState":"-1","articleType":"1","baiduIncludeResult":0,"baiduIncludeResultSearchNum":3,"baiduXueShuIncludeResult":0,"baiduXueShuIncludeResultSearchNum":0,"filename":"cg2020023.xml","googleIncludeResult":0,"googleIncludeResultSearchNum":0,"htmlSource":1,"htmlViewCount":305,"id":"3185dfdb-5da5-4a59-a8bc-ec618704f29d","isRegCstr":0,"isRegDOI":0,"isUpdate":"1","pdfDownCount":71,"pdfEnFileSizeInt":0,"pdfFileName":"cg2020023.pdf","pdfFileSize":24947.3,"pdfFileSizeInt":24947,"remark":"XML","viewCount":4213,"xmlDownCount":0,"xmlFileSize":60.68},"articleNo":"cg2020023","authors":[{"addressTagIds":"aff1","articleId":"8f885e29-71d0-4c75-88b5-b0fdf182d82a","authorNameCn":"","authorNameEn":"Xue-zhong Yu","authorTagVal":"a","authorType":"author","corresper":true,"correspinfoEn":"113606367@qq.com (Xue-zhong Yu)","email":"113606367@qq.com","givenNamesEn":"Xue-zhong","id":"25e8be14-8fcf-4626-aad4-47496ad9b015","sortNumber":1,"surNameEn":"Yu"},{"addressTagIds":"aff1","articleId":"8f885e29-71d0-4c75-88b5-b0fdf182d82a","authorNameCn":"","authorNameEn":"Yi-yuan He","authorTagVal":"a","authorType":"author","corresper":false,"givenNamesEn":"Yi-yuan","id":"cd14826d-dc2b-4ce4-89ef-3611a8878487","sortNumber":2,"surNameEn":"He"},{"addressTagIds":"aff1","articleId":"8f885e29-71d0-4c75-88b5-b0fdf182d82a","authorNameCn":"","authorNameEn":"Meng Wang","authorTagVal":"a","authorType":"author","corresper":false,"givenNamesEn":"Meng","id":"4e756edb-54a5-4872-9f0e-b2b7e33eda36","sortNumber":3,"surNameEn":"Wang"},{"addressTagIds":"aff2","articleId":"8f885e29-71d0-4c75-88b5-b0fdf182d82a","authorNameCn":"","authorNameEn":"Jian Zhang","authorTagVal":"b","authorType":"author","corresper":false,"givenNamesEn":"Jian","id":"c88b32af-537e-4af9-a3e4-467b191fc07d","sortNumber":4,"surNameEn":"Zhang"},{"addressTagIds":"aff1","articleId":"8f885e29-71d0-4c75-88b5-b0fdf182d82a","authorNameCn":"","authorNameEn":"Xuan-jie Zhang","authorTagVal":"a","authorType":"author","corresper":false,"givenNamesEn":"Xuan-jie","id":"cdb97396-1ba4-470a-bc62-e0ebd3791e2d","sortNumber":5,"surNameEn":"Zhang"},{"addressTagIds":"aff1","articleId":"8f885e29-71d0-4c75-88b5-b0fdf182d82a","authorNameCn":"","authorNameEn":"Zheng-guo Fan","authorTagVal":"a","authorType":"author","corresper":false,"givenNamesEn":"Zheng-guo","id":"807fcdca-13ae-482e-94fe-64656dc573ab","sortNumber":6,"surNameEn":"Fan"}],"categoryNameEn":"Original Articles","citationCn":"","citationEn":"Yu Xue-zhong, He Yi-yuan, Wang Meng, Zhang Jian, Zhang Xuan-jie, Fan Zheng-guo. 2020. Gravity and magnetic field characteristics and regional ore prospecting of the Yili ancient continent, West Tianshan, Xinjiang Uygur Autonomous Region, China. China Geology, 3(1), 104‒112. doi: 10.31035/cg2020023.","doi":"10.31035/cg2020023","figList":[{"dataId":"8f885e29-71d0-4c75-88b5-b0fdf182d82a","fileFrom":"xml","fileLastName":"jpg","filePath":"/fileZGDZYW/journal/article/zgdzyw/2020/1/cg2020023-1.jpg","fileSize":"633KB","fileType":"fulltextFig","fileXMLPath":"cg2020023-1.jpg","id":"9926d962-c82e-47ef-b547-219eab7afbd6","journalId":"ff007540-a7c7-4752-b593-efa08309babb","labelText":"1","nameEn":"Major geotectonic units in the eastern region of West Tianshan, Xinjiang Uygur Autonomous Region (modified from Qian Q et al., 2009). 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NNF–North Nalati fault; NTF–North Tarim fault; NTSZ–North Tianshan suture zone.","referSecTagIds":"","sort":0,"supplementRemarkCn":"","supplementRemarkEn":"","tagId":"Figure1","type":"article","typesetSecTagId":"s03","viewNum":0},"hasPage":true,"htmlAccess":true,"id":"8f885e29-71d0-4c75-88b5-b0fdf182d82a","issue":"1","issueArticle":"0","keywords":[{"articleId":"8f885e29-71d0-4c75-88b5-b0fdf182d82a","id":"8bc59e9f-5368-41bd-9904-ba53d92dc3cb","keywordEn":"Yili ancient continent","sortNum":1},{"articleId":"8f885e29-71d0-4c75-88b5-b0fdf182d82a","id":"9f15c462-20b4-4af4-a382-256634156fea","keywordEn":"Yili Carboniferous-Permian rift","sortNum":2},{"articleId":"8f885e29-71d0-4c75-88b5-b0fdf182d82a","id":"e6e376c7-ba29-48e7-b3ab-926075e692d3","keywordEn":"Gravity field","sortNum":3},{"articleId":"8f885e29-71d0-4c75-88b5-b0fdf182d82a","id":"d5d5b205-15f0-4932-9f8f-ccd1009750f0","keywordEn":"Epithermal gold deposit","sortNum":4},{"articleId":"8f885e29-71d0-4c75-88b5-b0fdf182d82a","id":"eb9e9f18-6716-4d50-b763-b5189e1309d5","keywordEn":"Copper polymetallic deposit","sortNum":5},{"articleId":"8f885e29-71d0-4c75-88b5-b0fdf182d82a","id":"c69a1915-f18e-41a7-9da7-b0f48fe70a31","keywordEn":"Geophysical and remote sensing survey engineering","sortNum":6},{"articleId":"8f885e29-71d0-4c75-88b5-b0fdf182d82a","id":"2867b8e7-8d08-4e45-b7e7-a955c4ed7cac","keywordEn":"Xinjiang Uygur Autonomous Region","sortNum":7},{"articleId":"8f885e29-71d0-4c75-88b5-b0fdf182d82a","id":"5e7c1390-8fe4-433f-ad3f-f68435250bd5","keywordEn":"China","sortNum":8}],"language":"en","notes":[],"page":"104-112","pdfAccess":true,"publisherId":"cg2020023","releaseProgress":{"articleId":"8f885e29-71d0-4c75-88b5-b0fdf182d82a","lastReleaseTime":"2020-12-23 13:28","maxLastReleaseTime":"2020-12-23 13:28","minLastReleaseTime":"2020-03-31 18:18","otherReleaseList":[]},"releaseState":1,"searchSort":"20200001000000","subTitleCn":"","subTitleEn":"","supplements":[],"tableList":[],"tags":[{"data":"{\"publisherId\":\"\",\"journalName\":\"\",\"remark\":\"\",\"createDate\":\"\",\"createUser\":\"\",\"status\":\"1\"}","id":"0","journalId":"ff007540-a7c7-4752-b593-efa08309babb","level":1,"nameCn":"轮播推荐","nameEn":"轮播推荐","outputName":"0","sort":0,"tags":[],"type":"recommend"}],"titleCn":"","titleEn":"Gravity and magnetic field characteristics and regional ore prospecting of the Yili ancient continent, West Tianshan, Xinjiang Uygur Autonomous Region, China","volume":"3","year":"2020","yearInt":2020},"dataId":"8f885e29-71d0-4c75-88b5-b0fdf182d82a","dataType":"Article","id":"8f885e29-71d0-4c75-88b5-b0fdf182d82a0","language":"en","sort":4,"tagId":"0"},{"data":{"abstractAccess":true,"abstractinfoCn":"","abstractinfoEn":"As the important component of the eastern Tethys tectonic region, the Jinsha River-Ailao Mountain suture zone is often considered to be an ophiolitic mélange belt. However, the P-T-t path and chronological framework of the metamorphic evolution in the collisional orogenetic process of this zone are still poorly understood owing to the lack of metamorphism research of symbolic high-pressure rocks. During a regional geological survey on a scale of 1∶50000 in Gonjo County, Xizang Autonomous Region involved in this paper, (retrograde) eclogites lenses of different scales were found in Jinsha River suture zone, eastern Xizang for the first time. The (retrograde) eclogites can be divided into garnet-albite-chlorite-actinolite schists and eclogites according to retrograde degrees. The mainly mineral components of eclogites include garnet (45%–50%), clinopyroxene (about 25%), and hornblende (5%–10%) primarily, and biotite, quartz, rutile, and muscovite secondarily. According to the data of electron probe micro analysis (EPMA), clinopyroxenes feature high content of Na2O (5.6%–6%) and corresponding jadeite (Jd) molecules of 37%–44%, and they fall within the omphacite region in Quad-Jd-Ae diagram. The temperature and pressure of the metamorphism at peak are P≈2.2–2.34 GPa and T≈622–688 °C respectively as measured with geobarometry Grt-Omp-Phe and geothermometer Grt-Omp. This will provide a new reference for the understanding of Paleo-Tethyan evolution. In this paper, two samples of eclogites were chosen for LA-ICP-MS zircon U-Pb dating and their 206Pb/238U ages obtained are 240 ± 3 Ma and 244 ± 1 Ma respectively. Furthermore, the zircons feature extremely low Th/U ratio (<0.01), extremely low content of Nb, Ta, and HREE, and invisible negative Eu anomaly. Therefore, the genesis of the zircons shall be eclogites-facies metamorphism, indicating that the 240–245 Ma determined in this paper shall be the age of eclogites-facies metamorphism and may represent the westward subduction-collision epoch of Paleo-Tethys Ocean located between Zhongza Block and Qamdo Block.","appendixList":[],"articleBusiness":{"articleId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","articleState":"-1","articleType":"1","baiduIncludeResult":0,"baiduIncludeResultSearchNum":3,"baiduXueShuIncludeResult":0,"baiduXueShuIncludeResultSearchNum":0,"filename":"cg2020003.xml","googleIncludeResult":0,"googleIncludeResultSearchNum":0,"htmlSource":1,"htmlViewCount":386,"id":"bade484d-b6d0-4efb-add3-6053c162177b","isRegCstr":0,"isRegDOI":0,"isUpdate":"1","pdfDownCount":350,"pdfEnFileSizeInt":0,"pdfFileName":"cg2020003.pdf","pdfFileSize":4790.34,"pdfFileSizeInt":4790,"remark":"XML","viewCount":5221,"xmlDownCount":0,"xmlFileSize":351.51},"articleNo":"cg2020003","authors":[{"addressTagIds":"aff1","articleId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","authorNameCn":"","authorNameEn":"Yuan Tang","authorTagVal":"a","authorType":"author","corresper":true,"correspinfoEn":"tyvienna@163.com (Yuan Tang)","email":"tyvienna@163.com","givenNamesEn":"Yuan","id":"cde1786b-2524-494e-9358-a5ce89c420ab","sortNumber":1,"surNameEn":"Tang"},{"addressTagIds":"aff1","articleId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","authorNameCn":"","authorNameEn":"Ya-dong Qin","authorTagVal":"a","authorType":"author","corresper":false,"givenNamesEn":"Ya-dong","id":"233afba1-ae9e-4fc2-8eb5-715958740d6f","sortNumber":2,"surNameEn":"Qin"},{"addressTagIds":"aff1","articleId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","authorNameCn":"","authorNameEn":"Xiao-dong Gong","authorTagVal":"a","authorType":"author","corresper":false,"givenNamesEn":"Xiao-dong","id":"99a8daf7-5f73-4cc4-b75d-3e6d50fb55c2","sortNumber":3,"surNameEn":"Gong"},{"addressTagIds":"aff1","articleId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","authorNameCn":"","authorNameEn":"Yao-yao Duan","authorTagVal":"a","authorType":"author","corresper":false,"givenNamesEn":"Yao-yao","id":"c3583b80-87b2-44d5-90af-613a89db39cf","sortNumber":4,"surNameEn":"Duan"},{"addressTagIds":"aff2","articleId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","authorNameCn":"","authorNameEn":"Gang Chen","authorTagVal":"b","authorType":"author","corresper":false,"givenNamesEn":"Gang","id":"e608b015-75b5-435f-99ff-0aa9b36d6dac","sortNumber":5,"surNameEn":"Chen"},{"addressTagIds":"aff2","articleId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","authorNameCn":"","authorNameEn":"Hong-you Yao","authorTagVal":"b","authorType":"author","corresper":false,"givenNamesEn":"Hong-you","id":"e8fe07b1-6744-4e22-b120-ff33e4ae1253","sortNumber":6,"surNameEn":"Yao"},{"addressTagIds":"aff3","articleId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","authorNameCn":"","authorNameEn":"Jun-xiong Liao","authorTagVal":"c","authorType":"author","corresper":false,"givenNamesEn":"Jun-xiong","id":"e81abce1-55dd-4873-b64a-208c437d8033","sortNumber":7,"surNameEn":"Liao"},{"addressTagIds":"aff4","articleId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","authorNameCn":"","authorNameEn":"Shi-yong Liao","authorTagVal":"d","authorType":"author","corresper":false,"givenNamesEn":"Shi-yong","id":"fbdb0840-4269-401b-b664-3ed3a2cc0395","sortNumber":8,"surNameEn":"Liao"},{"addressTagIds":"aff1","articleId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","authorNameCn":"","authorNameEn":"Dong-bing Wang","authorTagVal":"a","authorType":"author","corresper":false,"givenNamesEn":"Dong-bing","id":"8a1d9a78-101a-44b3-b706-6c8724f0d9b1","sortNumber":9,"surNameEn":"Wang"},{"addressTagIds":"aff1","articleId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","authorNameCn":"","authorNameEn":"Bao-di Wang","authorTagVal":"a","authorType":"author","corresper":false,"givenNamesEn":"Bao-di","id":"48ee8ddf-da14-4e5c-9e8f-567380dcd7dc","sortNumber":10,"surNameEn":"Wang"}],"categoryNameEn":"Original Articles","citationCn":"2020: Discovery of eclogites in Jinsha River suture zone, Gonjo County, eastern Xizang and its restriction on Paleo-Tethyan evolution. 中国地质(英文版), 3(1): 83-103. DOI: 10.31035/cg2020003","citationEn":"Tang Yuan, Qin Ya-dong, Gong Xiao-dong, Duan Yao-yao, Chen Gang, Yao Hong-you, Liao Jun-xiong, Liao Shi-yong, Wang Dong-bing, Wang Bao-di. 2020. Discovery of eclogites in Jinsha River suture zone, Gonjo County, eastern Xizang and its restriction on Paleo-Tethyan evolution. China Geology, 3(1), 83‒103. doi: 10.31035/cg2020003.","doi":"10.31035/cg2020003","figList":[{"dataId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","fileFrom":"xml","fileLastName":"jpg","filePath":"/fileZGDZYW/journal/article/zgdzyw/2020/1/cg2020003-1.jpg","fileSize":"2214KB","fileType":"fulltextFig","fileXMLPath":"cg2020003-1.jpg","id":"f970e51f-200b-48aa-8401-48f97fc3c762","journalId":"ff007540-a7c7-4752-b593-efa08309babb","labelText":"1","nameEn":"Simplified tectonic map with age data, showing the Paleo-Tethyan system in Xizang and adjacent area (after Xu ZQ et al., 2015).","referSecTagIds":"","sort":0,"supplementRemarkCn":"","supplementRemarkEn":"Blocks and terranes: NCB–North China Block; SCB– South China Block; TRMB–Tarim Block; IDB–India Block; EKL-QDM-QL–East Kunlun-Qaidam-Qilian terrane; WKL–West Kunlun terrane; SPGZ–Songpan-Ganze terrane; NQT-QD-SM-IC–North Qiangtang-Qamdo-Simao-Indochina terrane; SQT-BS-SB–South Qiangtang-Baoshan-Sibumasu terrane; NLS–North Lhasa terrane; SLS–South Lhasa terrane; TC–Tengchong terrane; TSH–Tianshuihai terrane; WB–West Burma terrane. Suture zones: EKL-ANMQS–East Kunlun-A’nyemaqen Suture; WKLS–West Kunlun Suture; LTS–Litang Suture; JSJ-ALS-SMS–Jinshajiang-Ailaoshan-Song Ma Suture; LS-CM-INS–Longmu Tso Shuanghu-Changning Menglian-Inthanon Suture; JH-NU-SKS–Jinghong-Nan Uttaradit-Sra Kaeo Suture; BNS–Bangonghu-Nujiang Suture; SQH-JLS–Siquanhe-Jiali Suture; SDS–Sumdo Suture; ITS–Indus-Tsangbo Suture; YD–Yidun Arc. Arc terranes: BHDA–Bulhanbuda Arc terrane; YDA–Yidun Arc terrane; LC-ST-CBA–Lincang-Sukhothai-Chanthaburi Arc terrane; KHA–Kohistan Arc terrane; LDA–Ladakh Arc terrane; WQL–West Qinglin terrane. Faults: ALTF–Altyn Tagh Fault; NQLT–North Qilian Thrust; LMST–Longmenshan Thrust; RRF–Red River Fault; KKF–Karakurum Fault; MFT–Main Frontal Thrust; SGF–Sagaing Fault; GLGF–Gaoligong Fault.","tagId":"Figure1","type":"article","typesetSecTagId":"s01","viewNum":0},{"dataId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","fileFrom":"xml","fileLastName":"jpg","filePath":"/fileZGDZYW/journal/article/zgdzyw/2020/1/cg2020003-2.jpg","fileSize":"3514KB","fileType":"fulltextFig","fileXMLPath":"cg2020003-2.jpg","id":"eb8b638b-083f-42d5-bd3f-57498f81ce45","journalId":"ff007540-a7c7-4752-b593-efa08309babb","labelText":"2","nameEn":"a–Geotectonic schematic map of Jinsha River suture zone (after Li XZ et al., 1999); b–generalized geological map of Jinsha River suture zone, Gonjo, Eastern Xizang (its location is shown in Fig. 2a).","referSecTagIds":"","sort":1,"supplementRemarkCn":"","supplementRemarkEn":"","tagId":"Figure2","type":"article","typesetSecTagId":"s02","viewNum":0},{"dataId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","fileFrom":"xml","fileLastName":"jpg","filePath":"/fileZGDZYW/journal/article/zgdzyw/2020/1/cg2020003-3.jpg","fileType":"fulltextFig","fileXMLPath":"cg2020003-3.jpg","id":"7ee854d2-699d-415e-8122-db8ed73b8e89","journalId":"ff007540-a7c7-4752-b593-efa08309babb","labelText":"3","nameEn":"Field occurrence characteristics of retrograde eclogites. a–d–retrograde eclogites occurring in the shape of lens; e–chlorite retrograded from garnet; f–white rim structure (yellow arrow) developed around a part of garnets; g–eclogites with low retrograde metamorphism.","referSecTagIds":"","sort":2,"supplementRemarkCn":"","supplementRemarkEn":"","tagId":"Figure3","type":"article","typesetSecTagId":"s03","viewNum":0},{"dataId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","fileFrom":"xml","fileLastName":"jpg","filePath":"/fileZGDZYW/journal/article/zgdzyw/2020/1/cg2020003-4.jpg","fileSize":"2863KB","fileType":"fulltextFig","fileXMLPath":"cg2020003-4.jpg","id":"4987bb9c-3099-4f15-b3a0-4e9d057044a6","journalId":"ff007540-a7c7-4752-b593-efa08309babb","labelText":"4","nameEn":"Microscopic characteristics of garnet-albite-chlorite actinolite (cross-polarized light). a–residual garnets and small chlorite + albite + actinolite compose symplectites, and retrograde reaction rim; b–residual pyroxene. Grt–garnet, Chl–chlorite, Ab–albite, Act–actinolite, Cpx–clinopyroxene.","referSecTagIds":"","sort":3,"supplementRemarkCn":"","supplementRemarkEn":"","tagId":"Figure4","type":"article","typesetSecTagId":"s04","viewNum":0},{"dataId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","fileFrom":"xml","fileLastName":"jpg","filePath":"/fileZGDZYW/journal/article/zgdzyw/2020/1/cg2020003-5.jpg","fileSize":"5443KB","fileType":"fulltextFig","fileXMLPath":"cg2020003-5.jpg","id":"73b63f20-d301-4d5d-a836-a3c83a1eb044","journalId":"ff007540-a7c7-4752-b593-efa08309babb","labelText":"5","nameEn":"Microscopic characteristics of eclogites (a, c–cross-polarized light; b, d–plane-polarized light); cracks visible and fine mineral inclusions developing in garnet crystals; omphacite hypautomorphic columnar in shape and sub-amphibolized, with rutile inclusions visible inside garnet grains. Grt–garnet, Omp–omphacite, Amp–hornblende, Bt–biotite, Qz–quartz, Ms–muscovite, Ru–rutile, red arrows indicates blue-green hornblendes growing around the garnet.","referSecTagIds":"","sort":4,"supplementRemarkCn":"","supplementRemarkEn":"","tagId":"Figure5","type":"article","typesetSecTagId":"s04","viewNum":0},{"dataId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","fileFrom":"xml","fileLastName":"jpg","filePath":"/fileZGDZYW/journal/article/zgdzyw/2020/1/cg2020003-6.jpg","fileSize":"3893KB","fileType":"fulltextFig","fileXMLPath":"cg2020003-6.jpg","id":"f6be4b32-646c-45ef-8381-ed8eb294195e","journalId":"ff007540-a7c7-4752-b593-efa08309babb","labelText":"6","nameEn":"SEM images of eclogites. a–garnet with radial cracks and phengite occurring among cracks in the fine foliaceous shape; b–worm-like fine grains generating omphacite rim owing to decompression and decomposition; c–rutile in xenomorphic granular shape; d–diagram of garnet components obtained by EPMA. Grt–garnet, Omp–omphacite, Phg–phengite, Ru–rutile.","referSecTagIds":"","sort":5,"supplementRemarkCn":"","supplementRemarkEn":"","tagId":"Figure6","type":"article","typesetSecTagId":"s04","viewNum":0},{"dataId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","fileFrom":"xml","fileLastName":"jpg","filePath":"/fileZGDZYW/journal/article/zgdzyw/2020/1/cg2020003-7.jpg","fileSize":"951KB","fileType":"fulltextFig","fileXMLPath":"cg2020003-7.jpg","id":"f24cc4e4-cded-4b18-baef-a33825333cce","journalId":"ff007540-a7c7-4752-b593-efa08309babb","labelText":"7","nameEn":"a–Quad-Jd-Ae compositional diagram of clinopyroxene, showing all testing points falling within the omphacite region; b–characteristics of Raman spectra of clinopyroxene in the eclogites, having the characteristic spectral peaks of omphacite; c–end-member composition diagramof garnet, showing testing points falling within the area of class-C garnet; d–garnet composition diagram; e–f–hornblende composition diagram, showing testing pointsfalling within subclasses magnesiohornblende and achromaite (a, after Morimoto N et al., 1988; c, after Coleman RG et al., 1965; e–f, after Leake BE et al., 1997).","referSecTagIds":"","sort":6,"supplementRemarkCn":"","supplementRemarkEn":"","tagId":"Figure7","type":"article","typesetSecTagId":"s05","viewNum":0},{"dataId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","fileFrom":"xml","fileLastName":"jpg","filePath":"/fileZGDZYW/journal/article/zgdzyw/2020/1/cg2020003-8.jpg","fileSize":"1175KB","fileType":"fulltextFig","fileXMLPath":"cg2020003-8.jpg","id":"ba851cd4-4589-4a99-b443-e3a97defdedf","journalId":"ff007540-a7c7-4752-b593-efa08309babb","labelText":"8","nameEn":"Partial CL images of zircons in eclogites and their hosting rocks.","referSecTagIds":"","sort":7,"supplementRemarkCn":"","supplementRemarkEn":"","tagId":"Figure8","type":"article","typesetSecTagId":"s06","viewNum":0},{"dataId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","fileFrom":"xml","fileLastName":"jpg","filePath":"/fileZGDZYW/journal/article/zgdzyw/2020/1/cg2020003-9.jpg","fileSize":"1842KB","fileType":"fulltextFig","fileXMLPath":"cg2020003-9.jpg","id":"c6a10cd3-57eb-4c29-8095-c0fc18bcdae6","journalId":"ff007540-a7c7-4752-b593-efa08309babb","labelText":"9","nameEn":"a–U-Pb age of zircons in sample D0521-4; b–cumulative gaussian and histogram plots of zircons in sample D0521-4; c–U-Pb concordant diagrams of zircons in sample D0521-1; d–contents of Th and U and Th/U ratios of zircons in samples D0521-4 and D0521-1; e–f–REE chondrite normalized diagram of in situ single zircon in samples D0521-4 and D0521-1. 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Suture zones: EKL-ANMQS–East Kunlun-A’nyemaqen Suture; WKLS–West Kunlun Suture; LTS–Litang Suture; JSJ-ALS-SMS–Jinshajiang-Ailaoshan-Song Ma Suture; LS-CM-INS–Longmu Tso Shuanghu-Changning Menglian-Inthanon Suture; JH-NU-SKS–Jinghong-Nan Uttaradit-Sra Kaeo Suture; BNS–Bangonghu-Nujiang Suture; SQH-JLS–Siquanhe-Jiali Suture; SDS–Sumdo Suture; ITS–Indus-Tsangbo Suture; YD–Yidun Arc. Arc terranes: BHDA–Bulhanbuda Arc terrane; YDA–Yidun Arc terrane; LC-ST-CBA–Lincang-Sukhothai-Chanthaburi Arc terrane; KHA–Kohistan Arc terrane; LDA–Ladakh Arc terrane; WQL–West Qinglin terrane. Faults: ALTF–Altyn Tagh Fault; NQLT–North Qilian Thrust; LMST–Longmenshan Thrust; RRF–Red River Fault; KKF–Karakurum Fault; MFT–Main Frontal Thrust; SGF–Sagaing Fault; GLGF–Gaoligong Fault.","tagId":"Figure1","type":"article","typesetSecTagId":"s01","viewNum":0},"hasPage":true,"htmlAccess":true,"id":"d525bc6d-f970-4b10-95a2-30917b13d9c4","issue":"1","issueArticle":"0","keywords":[{"articleId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","id":"30ac8270-38ff-4e81-80a3-515df59b95e5","keywordEn":"Eclogite","sortNum":1},{"articleId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","id":"a24b382d-6790-4834-b26f-04908e59fee4","keywordEn":"Omphacite","sortNum":2},{"articleId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","id":"cdc5f062-0bc5-4fda-9971-cf1c96c13272","keywordEn":"Jinsha River suture zone","sortNum":3},{"articleId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","id":"d5d38d28-a485-4707-8120-9b861a6bfa28","keywordEn":"Geological survey engineering","sortNum":4},{"articleId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","id":"1ed84778-5620-4100-94b3-4d2efe4f90c7","keywordEn":"Qinghai-Xizang plateau","sortNum":5},{"articleId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","id":"3df7b9e9-403c-49c7-bbee-143cc58b0e3f","keywordEn":"Eastern Xizang","sortNum":6},{"articleId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","id":"42e80ba4-c060-4b4c-86cf-35a1425256f4","keywordEn":"China","sortNum":7}],"language":"en","notes":[],"page":"83-103","pdfAccess":true,"publisherId":"cg2020003","releaseProgress":{"articleId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","lastReleaseTime":"2020-12-23 10:43","maxLastReleaseTime":"2020-12-23 10:43","minLastReleaseTime":"2020-03-31 18:18","otherReleaseList":[{"articleId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","currentState":"Accepted Manuscript","currentStateEn":"Accepted Manuscript","lastReleaseTime":"2020-03-25 14:18","maxLastReleaseTime":"2020-03-25 14:18","minLastReleaseTime":"2020-03-18 19:12","otherReleaseList":[]}]},"releaseState":1,"searchSort":"20200001000000","subTitleCn":"","subTitleEn":"","supplements":[],"tableList":[],"tags":[{"data":"{\"publisherId\":\"\",\"journalName\":\"\",\"remark\":\"\",\"createDate\":\"\",\"createUser\":\"\",\"status\":\"1\"}","id":"0","journalId":"ff007540-a7c7-4752-b593-efa08309babb","level":1,"nameCn":"轮播推荐","nameEn":"轮播推荐","outputName":"0","sort":0,"tags":[],"type":"recommend"}],"titleCn":"Discovery of eclogites in Jinsha River suture zone, Gonjo County, eastern Xizang and its restriction on Paleo-Tethyan evolution","titleEn":"Discovery of eclogites in Jinsha River suture zone, Gonjo County, eastern Xizang and its restriction on Paleo-Tethyan evolution","volume":"3","year":"2020","yearInt":2020},"dataId":"d525bc6d-f970-4b10-95a2-30917b13d9c4","dataType":"Article","id":"d525bc6d-f970-4b10-95a2-30917b13d9c40","language":"en","sort":5,"tagId":"0"},{"data":{"abstractAccess":true,"abstractinfoCn":"","abstractinfoEn":"The giant potash deposit on the Khorat Plateau is one of the most promising targets for exploitation of potassium salts. So far, many researches and geologic survey have been conducted on the giant potash deposits. Hence, it is necessary to make an overall review on the potash deposits. The potash deposit on the Khorat Plateau was formed during the Middle to Late Cretaceous, during which seawater was enriched in Ca2+ and depleted in SO42- compared with those of modern seawater. In addition to seawater, continental water and hydrothermal fluids could have affected the evaporite basins. The seawater was probably derived from Tethys ocean, and the brine should have evaporated to some extent before entering into the basin systems based on the evidence of absence of carbonates and unproportionate sulphate compared with chloride salts. The paleo-climate during Middle to Late Cretaceous was characterized as high temperature and extremely arid environment, which is favourable for deposition of potassium-magnesium saline minerals. The major saline minerals are of anhydrite, halite, carnallite, sylvite and, tachyhydrite, with trace amounts of borates. The resources of the potash deposit on the Khorat Plateau could be approximately as much as 400×109 t of carnallite and 7×109 t of sylvite. The evaporite sequences have been deformed and altered by postdepositinal processes, including tectonic movements and chemical alteration. Salt domes were formed in the postdepositional processes. Based on the analyses of geophysical surveys and drilling projects, high-quality sylvinite ores are commonly found at the flanks of those salt domes due to incongruent dissolution of carnallite. The future potential prospecting areas for the high-quality sylvinite ores would be on the edges of the Khorat Plateau.","appendixList":[],"articleBusiness":{"articleId":"93ca32f6-c9cf-44ff-838c-48495dd29c28","baiduIncludeResult":0,"baiduIncludeResultSearchNum":3,"baiduXueShuIncludeResult":0,"baiduXueShuIncludeResultSearchNum":0,"filename":"cg2020009.xml","googleIncludeResult":0,"googleIncludeResultSearchNum":0,"htmlSource":1,"htmlViewCount":321,"id":"d32cefc3-df26-48f7-8b4d-2029ab241922","isRegCstr":0,"isRegDOI":0,"isUpdate":"1","pdfDownCount":109,"pdfEnFileSizeInt":0,"pdfFileName":"cg2020009.pdf","pdfFileSize":16936.05,"pdfFileSizeInt":16936,"viewCount":4341,"xmlFileSize":110.99},"articleNo":"cg2020009","authors":[{"addressTagIds":"aff1","articleId":"93ca32f6-c9cf-44ff-838c-48495dd29c28","authorNameCn":"","authorNameEn":"Li-jian Shen","authorTagVal":"a","authorType":"author","corresper":true,"correspinfoEn":"shenlijian1019@126.com (Li-jian Shen)","email":"shenlijian1019@126.com","givenNamesEn":"Li-jian","id":"868bef02-666a-4cf1-b24d-5427e6b65ef8","sortNumber":1,"surNameEn":"Shen"},{"addressTagIds":"aff2","articleId":"93ca32f6-c9cf-44ff-838c-48495dd29c28","authorNameCn":"","authorNameEn":"Nuchit Siritongkham","authorTagVal":"b","authorType":"author","corresper":false,"givenNamesEn":"Nuchit","id":"eba84021-0ee3-4311-b2cb-3b1ec05397f6","sortNumber":2,"surNameEn":"Siritongkham"}],"categoryNameEn":"Original Articles","citationCn":"","citationEn":"Shen Li-jian, Siritongkham Nuchit. 2020. The characteristics, formation and exploration progress of the potash deposits on the Khorat Plateau, Thailand and Laos, Southeast Asia. China Geology, 3(1), 67‒82. doi: 10.31035/cg2020009.","doi":"10.31035/cg2020009","figList":[{"dataId":"93ca32f6-c9cf-44ff-838c-48495dd29c28","fileFrom":"xml","fileLastName":"jpg","filePath":"/fileZGDZYW/journal/article/zgdzyw/2020/1/cg2020009-1.jpg","fileSize":"3705KB","fileType":"fulltextFig","fileXMLPath":"cg2020009-1.jpg","id":"37dd2174-6d23-48da-ba41-3db7804d0698","journalId":"ff007540-a7c7-4752-b593-efa08309babb","labelText":"1","nameEn":"The distribution of the Khorat Basin and Sakon Nakhon Basin on the Khorat Plateau (from Google Earth). a–location of the Khorat Plateau; b–distribution of the Sakon Nakhon Basin and the Khorat 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\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t

Resource: Ministry of Natural Resources

China Mineral Resources 2013.pdf


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China Geology创刊于2018年，是由中国地质调查局主管，中国地质调查局和中国地质科学院联合主办的地学综合英文OA期刊，旨在立足国内外地质调查成果，搭建国际高水平地质调查成果交流平台，满足人类社会对地质和矿产资源需求，引领世界地质学科发展新方向。

期刊内容涵盖以解决国计民生为导向的重大地质科技成果（矿产地质、能源地质、工程地质、地质灾害、水文地质、环境地质、气候变化等），兼及基础地质理论与新发现为导向的创新成果（岩石矿物、构造地质、地球化学、同位素地质、沉积古生物、海洋地质等）。期刊分为四个栏目：原创学术论文（Original Articles）、综述学术论文（Review Articles）、发现与进展（Short Communicatons）、简讯与新闻（News and Highlights）。

目前本刊已被ESCI、SCOPUS、DOAJ、ScienceDirect、CSCD、中国科技核心、CNKI、万方等国内外44个数据库和机构所收录。2022年6月获得 Scopus数据库的CiteScore引用分4.9分，在地质学（Geology）、古生物学（Paleontology）、海洋学（Oceanography）、地表过程（Earth-Surface Processes）等多个学科分类中均位于Q1区； 2021年7月公布的WOS数据库JCR报告中，China Geology的JCI指数位于其收录的66种ESCI地球科学期刊中居第1名，在396种地学领域期刊（含SCIE和ESCI期刊）中居98位。

China Geology中英双语宣传片包括：China Geology创刊背景、China Geology是高水平研究成果展示的平台、China Geology是优秀学术人才成长的平台、China Geology是全球地质学术交流的平台、China Geology是地质知识国际传播的平台五个部分。

通过视频带您全方位了解China Geology。China Geology愿助您探索成就梦想，创新引领未来！


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China Geology中英双语宣传片重磅发布！"},"dataId":"22","dataType":"News","id":"96ee2f50-f072-44d7-b6f5-b50feea9a79e","language":"en","sort":8,"tagId":"0"},{"data":{"abstractAccess":true,"abstractinfoCn":"","abstractinfoEn":"Coal measure gas (also known as coal-bearing unconventional gas) is the key field and development direction of unconventional natural gas in recent years. The exploration and evaluation of coal measure gas (coalbed methane, coal shale gas and coal measure tight sandstone gas) from single coalbed methane has greatly expanded the field and space of resource evaluation, which is of positive significance for realizing the comprehensive utilization of coal resources, maximizing the benefits and promoting the innovation of oil and gas geological theory and technological advances in exploration and development. For the first time, in Yangmeishu Syncline of Western Guizhou Province, the public welfare coalbed methane geological survey project of China Geological Survey has been carried out a systematic geological survey of coal measure gas for the Upper Permian Longtan Formation, identified the geological conditions of coal measure gas and found high quality resources. The total geological resource quantity of coalbed methane and coal shale gas is 51.423×109 m3 and the geological resource abundance is up to 566×106 m3/km2. In this area, the coal measures are characterized by many layers of minable coal seams, large total thickness, thin to the medium thickness of the single layer, good gas-bearing property of coal seams and coal measure mudstone and sandstone, good reservoir physical property and high-pressure coefficient. According to the principle of combination of high quality and similarity of key parameters of the coal reservoir, the most favorable intervals are No.5–2, No.7 and No.13–2 coal seam in Well YMC1. And the pilot tests are carried out on coal seams and roof silty mudstone, such as staged perforation, increasing hydraulic fracturing scale and “three gas” production. The high and stable industrial gas flow with a daily gas output of more than 4000 m3 has been obtained, which has realized the breakthrough in the geological survey of coal measure gas in Southwest China. Based on the above investigation results, the geological characteristics of coal measure gas in the multi-thin-coal-seam-developed area and the co-exploration and co-production methods, such as the optimization method of favorable intervals, the high-efficiency fracturing and reservoir reconstruction method of coal measures, and the “three gas” drainage and production system, are systematically summarized in this paper. 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Resource: Ministry of Natural Resources

China Mineral Resources 2012.pdf

","downloadFile":"0","id":38,"imagePath":"","linkedWebsite":"","newsColumn":{"abbreviation":"data","breviaryShowNum":10,"columnNewsTemplate":"news_detail_en.vm","createTime":"2017-12-29 00:00:00","id":7,"journalId":"ff007540-a7c7-4752-b593-efa08309babb","language":"en","level":2,"mobileShow":1,"name":"Data","oldId":"4a9857d5-a394-4736-87ca-5f550677e373","openTarget":"_top","parent":{"abbreviation":"newsanddata","columnNewsTemplate":"news_detail_en.vm","createTime":"2017-12-29 00:00:00","id":17,"journalId":"ff007540-a7c7-4752-b593-efa08309babb","language":"en","level":1,"mobileShow":1,"name":"News & Data","oldId":"13712de2-f738-4442-8f43-73a3f9e1c68c","openTarget":"_top","showLocation":"1","sort":4,"state":"1","type":"1","updateTime":"2022-06-30 00:00:00","urlLink":"javascript:void(0);","urlLinkAPP":"javascript:void(0);"},"showLocation":"1","sort":1,"state":"1","type":"1","updateTime":"2022-07-12 00:00:00","urlLink":"","urlLinkAPP":""},"openTarget":"_top","outputName":"","releaseState":"publish","releaseTime":"2018-05-27 09:19:10","releaseYear":"2018","tags":[{"data":"{\"publisherId\":\"\",\"journalName\":\"\",\"remark\":\"\",\"createDate\":\"\",\"createUser\":\"\",\"status\":\"1\"}","id":"0","journalId":"ff007540-a7c7-4752-b593-efa08309babb","level":1,"nameCn":"轮播推荐","nameEn":"轮播推荐","outputName":"0","sort":0,"tags":[],"type":"recommend"}],"title":"China Mineral Resources 2012","titleEn":"","type":""},"dataId":"38","dataType":"News","id":"91d7d0ef-693e-4027-a9c5-0f1046aaca95","language":"en","sort":9,"tagId":"0"},{"data":{"abstractAccess":true,"abstractinfoCn":"","abstractinfoEn":"Bottom simulating reflector (BSR) has been recognized as one of the indicators of gas hydrates. However, BSR and hydrate are not one-to-one correspondence. In the Xisha area of South China Sea (SCS), carbonate rocks wildly develop, which continuously distribute parallel to the seafloor with high amplitude on seismic sections, exhibiting reflections similar to BSRs in the Shenhu area nearby. This phenomenon causes some interference to hydrates identification. In this paper, the authors discussed the typical geophysical differences between carbonate rocks and hydrates, indicating that the main difference exists in relationship between porosity and velocity, causing different amplitude versus offset (AVO) characters. Then the authors proposed a new model assuming that the carbonates form the matrix and the hydrate fill the pore as a part of the matrix. The key modeling parameters have been optimized constrained by P-velocities and S-velocities simultaneously, and the model works well both for carbonate rock and gas hydrate bearing sediments. For quantitative identification, the authors calculated the velocities when carbonates and hydrates form the matrix together in different proportions. Then they proposed a carbonate and hydrate identification template (CHIT), in which the possible hydrate saturation (PHS) and possible carbonate content (PCC) can be both scaled out for a group of sample composed by P-velocity and S-velocity. If PHS is far larger than PCC, it is more likely to be a hydrate sample because carbonates and hydrates do not coexist normally. The real data application shows that the template can effectively distinguish between hydrates and carbonate rocks, consequently reducing the risk of hydrate exploration.","appendixList":[],"articleBusiness":{"articleId":"d0883461-af7d-4490-9bf9-ce07eb96468c","articleState":"-1","articleType":"1","baiduIncludeResult":0,"baiduIncludeResultSearchNum":3,"baiduXueShuIncludeResult":0,"baiduXueShuIncludeResultSearchNum":0,"filename":"cg2020021.xml","googleIncludeResult":0,"googleIncludeResultSearchNum":0,"htmlSource":1,"htmlViewCount":360,"id":"5bb33663-5ab5-47b4-8484-cb8568fe8fc6","isRegCstr":0,"isRegDOI":0,"isUpdate":"1","pdfDownCount":166,"pdfEnFileSizeInt":0,"pdfFileName":"cg2020021.pdf","pdfFileSize":19108.22,"pdfFileSizeInt":19108,"remark":"XML","viewCount":4479,"xmlDownCount":0,"xmlFileSize":84.15},"articleNo":"cg2020021","authors":[{"addressTagIds":"aff1,aff2","articleId":"d0883461-af7d-4490-9bf9-ce07eb96468c","authorNameCn":"","authorNameEn":"Jin-qiang Liang","authorTagVal":"a,b","authorType":"author","corresper":true,"correspinfoEn":"ljinqiang@hydz.com (Jin-qiang Liang)","email":"ljinqiang@hydz.com","givenNamesEn":"Jin-qiang","id":"3dcdf7b1-4e82-42d3-a9ae-85e80f4ef0ec","sortNumber":1,"surNameEn":"Liang"},{"addressTagIds":"aff1,aff2","articleId":"d0883461-af7d-4490-9bf9-ce07eb96468c","authorNameCn":"","authorNameEn":"Wei Deng","authorTagVal":"a,b","authorType":"author","corresper":true,"correspinfoEn":"hahens@163.com (Wei Deng)","email":"hahens@163.com","givenNamesEn":"Wei","id":"c6c897c1-f9e7-48c2-806a-c1b4207f5806","sortNumber":2,"surNameEn":"Deng"},{"addressTagIds":"aff1","articleId":"d0883461-af7d-4490-9bf9-ce07eb96468c","authorNameCn":"","authorNameEn":"Jing-an Lu","authorTagVal":"a","authorType":"author","corresper":false,"givenNamesEn":"Jing-an","id":"1d8a3760-9879-4de6-a5d4-677dfa0d8432","sortNumber":3,"surNameEn":"Lu"},{"addressTagIds":"aff3","articleId":"d0883461-af7d-4490-9bf9-ce07eb96468c","authorNameCn":"","authorNameEn":"Zeng-gui Kuang","authorTagVal":"c","authorType":"author","corresper":false,"givenNamesEn":"Zeng-gui","id":"1920fb9a-ac60-4743-9620-a0f91db53adf","sortNumber":4,"surNameEn":"Kuang"},{"addressTagIds":"aff1,aff3","articleId":"d0883461-af7d-4490-9bf9-ce07eb96468c","authorNameCn":"","authorNameEn":"Yu-lin He","authorTagVal":"a,c","authorType":"author","corresper":false,"givenNamesEn":"Yu-lin","id":"4b0f73dd-318d-4f3e-ade8-304313a6f7c3","sortNumber":5,"surNameEn":"He"},{"addressTagIds":"aff2","articleId":"d0883461-af7d-4490-9bf9-ce07eb96468c","authorNameCn":"","authorNameEn":"Wei Zhang","authorTagVal":"b","authorType":"author","corresper":false,"givenNamesEn":"Wei","id":"10dd94b7-0880-418f-a357-6b24ddd9c192","sortNumber":6,"surNameEn":"Zhang"},{"addressTagIds":"aff1,aff2","articleId":"d0883461-af7d-4490-9bf9-ce07eb96468c","authorNameCn":"","authorNameEn":"Yue-hua Gong","authorTagVal":"a,b","authorType":"author","corresper":false,"givenNamesEn":"Yue-hua","id":"31eba4b8-fdef-490e-94bf-cbdc5b8db609","sortNumber":7,"surNameEn":"Gong"},{"addressTagIds":"aff1,aff2","articleId":"d0883461-af7d-4490-9bf9-ce07eb96468c","authorNameCn":"","authorNameEn":"Jin Liang","authorTagVal":"a,b","authorType":"author","corresper":false,"givenNamesEn":"Jin","id":"457e1723-e66b-4b76-ab1b-79fe15f7257b","sortNumber":8,"surNameEn":"Liang"},{"addressTagIds":"aff2,aff3","articleId":"d0883461-af7d-4490-9bf9-ce07eb96468c","authorNameCn":"","authorNameEn":"Miao-miao Meng","authorTagVal":"b,c","authorType":"author","corresper":false,"givenNamesEn":"Miao-miao","id":"e57cf5c3-b1ac-4725-a7ff-6be4338c2027","sortNumber":9,"surNameEn":"Meng"}],"categoryNameEn":"Original Articles","citationCn":"","citationEn":"Liang Jin-qiang, Deng Wei, Lu Jing-an, Kuang Zeng-gui, He Yu-lin, Zhang Wei, Gong Yue-hua, Liang Jin, Meng Miao-miao. 2020. A fast identification method based on the typical geophysical differences between submarine shallow carbonates and hydrate bearing sediments in the northern South China Sea. China Geology, 3(1), 16‒27. doi: 10.31035/cg2020021.","doi":"10.31035/cg2020021","figList":[{"dataId":"d0883461-af7d-4490-9bf9-ce07eb96468c","fileFrom":"xml","fileLastName":"jpg","filePath":"/fileZGDZYW/journal/article/zgdzyw/2020/1/cg2020021-1.jpg","fileSize":"4512KB","fileType":"fulltextFig","fileXMLPath":"cg2020021-1.jpg","id":"3ebb7fac-9de4-4e11-83b8-67e17bfbe771","journalId":"ff007540-a7c7-4752-b593-efa08309babb","labelText":"1","nameEn":"a–Location of the study areas; b–submarine landform map of SH area; c–submarine landform map of XS area.","referSecTagIds":"","sort":0,"supplementRemarkCn":"","supplementRemarkEn":"","tagId":"Figure1","type":"article","typesetSecTagId":"s01","viewNum":0},{"dataId":"d0883461-af7d-4490-9bf9-ce07eb96468c","fileFrom":"xml","fileLastName":"jpg","filePath":"/fileZGDZYW/journal/article/zgdzyw/2020/1/cg2020021-2.jpg","fileSize":"2313KB","fileType":"fulltextFig","fileXMLPath":"cg2020021-2.jpg","id":"ae7dc69b-1b88-4d7f-ae45-4483230d7ba5","journalId":"ff007540-a7c7-4752-b593-efa08309babb","labelText":"2","nameEn":"Typical BSRs in the SH on the post-stack seismic profile. 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On June 8, 2023, Elsevier's Scopus database updated the CiteScore 2022 metric for evaluating scholarly publications. This index provides the latest measurement of the citation impact of peer-reviewed journals, book series, conference papers and industry journals included in the Scopus database.

China Geology's CiteScore rises to 5.1 in 2022, ranking Q1 in the categories of geology (79th percentile) and earth-surface processes (77th percentile). Its citation rate has reached 85%. The SJR (SCImago Journal Rank) and SNIP (Source Normalized Impact per Paper) in 2022 are 0.728 and 1.484, respectively, which are higher than the 2021 metrics. It is worth noting that the journal’s CiteScoreTracker 2023 has reached 6, indicating that the CiteScore of China Geology is expected to increase significantly in 2023, signifying an even greater potential for growth.

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China Geology is a multidisciplinary geoscience journal published by the China Geological Survey and co-sponsored by the China Geological Survey and the Chinese Academy of Geological Sciences. It aims to build a world-class platform for the exchange of earth science and technology achievements, and promote the dissemination of local and overseas geoscience research results, latest research progress and related content. The journal primarily publishes new research results in multidisciplinary geosciences, together with traditional topics in geology. Topics include stratigraphy, paleontology, tectonics, petrology (igneous, metamorphic and sedimentology), geochemistry, mineralogy, petroleum geology, marine geology, hydrology, environmental geology, remote sensing, etc. Established in 2018, China Geology cooperates with KeAi Press to publish full-text OA on Elsevier’s ScienceDirect database. The journal indexed by 46 databases and institutions, including ESCI, Scopus, DOAJ, ScienceDirect, Geobase, Chemical Abstract Services, Referativnyi Zhurnal (Abstract Journal), Chinese Academy of Sciences CSCD, China Science and Technology Core Journal, CNKI, Wanfang Data, VIP Information, among many others.

     

Further Readings

Scopus

Your brilliance, connected.

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Scopus is a source-neutral abstract and citation database curated by independent subject matter experts who are recognized leaders in their fields. Scopus puts powerful discovery and analytics tools in the hands of researchers, librarians, research managers and funders to promote ideas, people and institutions.

 

Powered by Scopus and its 28,100+ active titles from 7000+ publishers across 333 disciplines, CiteScore provides transparent metrics that enable well-informed publishing strategy, library collection development and benchmarking of journal performance. CiteScore metrics enrich the evaluation of serial titles and provide transparent data to help you measure the citation impact for journals, book series, conference proceedings and trade journals.

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Independent Content Selection

The Scopus Content Selection and Advisory Board (CSAB) is an international group of scientists, researchers and librarians who represent the major scientific disciplines. Year round, the board members are responsible for reviewing all titles that are suggested to Scopus. For more information on Scopus Content Selection, please visit: https://www.elsevier.com/zh-cn/solutions/scopus


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To increase the journal’s global visibility, expand its author base and attract more high-quality content, China Geology releases an information leaflet for promotion of the journal in international academic events.

We encourage you to share the leaflet with your colleagues and students, and disseminate it during your visits, talks and conferences to spread the information about the journal. Thank you for your support of China Geology!

Download the leaflet

\"\"

\"\"

\t\t\t\t\t\t\t\t","downloadFile":"0","id":13,"imagePath":"","linkedWebsite":"","newsColumn":{"abbreviation":"news","breviaryShowNum":10,"columnNewsTemplate":"news_detail_en.vm","createTime":"2017-06-26 00:00:00","id":11,"journalId":"ff007540-a7c7-4752-b593-efa08309babb","language":"en","level":2,"mobileShow":1,"name":"News","oldId":"c3ca57d7-2bb4-47d5-a460-9d96d18f7671","openTarget":"_top","parent":{"abbreviation":"newsanddata","columnNewsTemplate":"news_detail_en.vm","createTime":"2017-12-29 00:00:00","id":17,"journalId":"ff007540-a7c7-4752-b593-efa08309babb","language":"en","level":1,"mobileShow":1,"name":"News & Data","oldId":"13712de2-f738-4442-8f43-73a3f9e1c68c","openTarget":"_top","showLocation":"1","sort":4,"state":"1","type":"1","updateTime":"2022-06-30 00:00:00","urlLink":"javascript:void(0);","urlLinkAPP":"javascript:void(0);"},"showLocation":"1","sort":2,"state":"1","type":"1","updateTime":"2018-06-06 00:00:00","urlLink":"","urlLinkAPP":""},"openTarget":"_top","releaseState":"publish","releaseTime":"2023-07-26 18:36:26","releaseYear":"2023","tags":[{"data":"{\"publisherId\":\"\",\"journalName\":\"\",\"remark\":\"\",\"createDate\":\"\",\"createUser\":\"\",\"status\":\"1\"}","id":"0","journalId":"ff007540-a7c7-4752-b593-efa08309babb","level":1,"nameCn":"轮播推荐","nameEn":"轮播推荐","outputName":"0","sort":0,"tags":[],"type":"recommend"}],"title":"China Geology Information Leaflet"},"dataId":"13","dataType":"News","id":"aa5ed7a8-7a06-4d54-b65b-c6d62c53e70b","language":"en","sort":13,"tagId":"0"},{"data":{"content":"\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t

The SinoProbe Center of the China Geological Survey is a professional institution for deep geological survey and deep process research, which is also the national base for deep exploration and deep earth science researches in China. It is mainly carried out deep explorations of the earth, deep geological surveys and fundamental researches on deep earth science. The Sinoprobe Center undertakes deep earth structural and compositional exploration, technology research and development on deep earth exploration, exploitation and evaluation of deep oil and gas, deep mineral resources, deep geothermal energy, and underground space exploration and utilization. It will provide technical support and data services in the field of deep earth to guarantee the national resources and energy security and development of the earth science. The director of the SinoProbe Center is Professor Guang-sheng Yan, and the deputy directors are professors Qing-tian Lv and Yan Ma.

\"http://www.sinoprobe.org/templates/main/sino2017/images/a2.jpg\"

Group photo of the Sinoprobe Center in Beijing, China.

 

There are 9 divisions of the SinoProbe Center as follows:

  1. 1.      Division of deep mineral resource exploration and evaluation

This division is based on geophysical technologies, multi-disciplinary and multi-deep exploration scales to reveal the deep processes, 3D structures, and metallogenic processing of the typical metallogenic belts or ore-concentrated areas in the deep earth. The division is aimed to construct regional metallogenic dynamics, discover innovative technologies and methods of geophysical data collection, processing, develop multi-data-based inversion and lithological recognition methods, and set up technical combined system of deep mineral deposits exploration.

  1. 2.      Division of deep oil and gas exploration and evaluation

This division is focused on deep and ultra-deep structure exploration of oil and gas potentials, evaluation of large-scaled orogenic petroliferous basin belts, and new oil and gas strata discoveries in the North China basins to further explore deep oil and gas resources.

  1. 3.      Division of underground space exploration and utilization

This division is aimed to carry out following technologies such as anti-interference high precision geophysical techniques, underground drilling and logging techniques with preciselocalization and monitoring techniques, risk assessment of active faulting for underground space exploration and utilization, multiple parameter information integration and AI modeling, collaborative planning and utilization of underground and ground spaces, dynamic information system of construction, maintenance of the urban underground space systems, utilization of underground caves and fractures, natural gas and energy storage, construction of underground self-circulation ecosystem, and monitoring evaluation system of underground space engineering.

  1. 4.      Division of geothermal energy and groundwater research

This division is concentrated on modeling evolution history of the tectonic controlled geothermal system studies, geophysical explorations, high temperature drilling and geothermal logging studies, and reservoir environments and re-injection technologies developments.

  1. 5.      Division of ultra-deep scientific drilling

This division is focused on general design and operation management of ultra-deep scientific drilling programs, developing ultra-deep drilling equipments, drilling technologies and materials, constructions of simulation laboratory for high P–T drilling and analysis center for drilling samples, and implementing scientific drilling programs for major geological problems in key areas.

  1. 6.      Division of deep earth science

This division is aimed to reveal the 3D structure, deep processes, and deep earth geodynamics of the continental lithosphere through structural and compositional explorations. Geophysical seismic profiling will be used to study tectonic boundaries and basement. The deep earth science division will use physical simulation of geological structures to study deformation mechanism and theories. Based on high P and T physical experiments with numerical modeling, the division will reveal deep earth processes such as partial melting, phase transition, material circulation (including deep carbon circulation), energy conversion, and rock and mineral rheology. Moreover, to carry out deep structural exploration and integration research on the uplift and growth, geodynamic evolution of the Xizang plateau, and its resource and environmental effects, the division will be highly concentrated on studying the Xizang plateau and surrounding basin-range junction belts.

  1. 7.      Division of data management and sharing

This division manages the submission, collection, integration, releasing and public sharing of the national big data on deep exploration,3D geodynamic modeling of the continental lithosphere, and 3D visualization of the deep earth.

  1. 8.      Division of large equipment operation and maintenance

This division is responsible for large equipment configuration, deployment, and regular maintenance. It will also provide standardization and coordination services of the equipments, sharing service to outside institutions. The division is in charge of executing the technical upgrade, renovation, and independent development of the deep exploration equipment. Annual equipment procurement plan and operating status report will be published from the large equipment division.

  1. 9.      Division of administration

The administration division is responsible for daily management, international cooperation, and public service.


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Emerging Sources Citation Index (ESCI)

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INSPEC

Cambridge Scientific Abstracts (CSA)

American Chemical Abstracts (CA)

Russian Abstracts Journal (AJ)

China Scientific and Technical Papers and Citation Database (CSTPCD)

Chinese Science Citation Database (CSCD)

J-Gate

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Geobase

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MIAR

Ulrich's Periodicals Directory



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