Origin of natural sulfur-metal chimney in the Tangyin hydrothermal field, Okinawa Trough: constraints from rare earth element and sulfur isotopic compositions

Hong Cao; Zhi-lei Sun; Chang-ling Liu; En-tao Liu; Xue-jun Jiang; Wei Huang

doi:10.31035/cg2018023

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Articles in press have been peer-reviewed and accepted, which are not yet edited and assigned to volumes/issues, but are citable by Digital Object Identifier (DOI).

Cao Hong, Sun Zhi-lei, Liu Chang-ling, Liu En-tao, Jiang Xue-jun, Huang Wei. 2018. Origin of natural sulfur-metal chimney in the Tangyin hydrothermal field, Okinawa Trough: constraints from rare earth element and sulfur isotopic compositions. China Geology, 1(2), 225‒235. doi: 10.31035/cg2018023.

Citation:

Cao Hong, Sun Zhi-lei, Liu Chang-ling, Liu En-tao, Jiang Xue-jun, Huang Wei. 2018. Origin of natural sulfur-metal chimney in the Tangyin hydrothermal field, Okinawa Trough: constraints from rare earth element and sulfur isotopic compositions. China Geology, 1(2), 225‒235. doi: 10.31035/cg2018023.

Citation:

Cao Hong, Sun Zhi-lei, Liu Chang-ling, Liu En-tao, Jiang Xue-jun, Huang Wei. 2018. Origin of natural sulfur-metal chimney in the Tangyin hydrothermal field, Okinawa Trough: constraints from rare earth element and sulfur isotopic compositions. China Geology, 1(2), 225‒235. doi: 10.31035/cg2018023.