Multiple mineralization events of the Paleozoic Tuwu porphyry copper deposit, Eastern Tianshan: evidence from geology, fluid inclusions, sulfur isotopes, and geochronology-Reference-Cited by-同舟云学术

Multiple mineralization events of the Paleozoic Tuwu porphyry copper deposit, Eastern Tianshan: evidence from geology, fluid inclusions, sulfur isotopes, and geochronology

Published:2018-12-19 Issue:7 Volume:54 Page:1053-1076
ISSN:0026-4598
Container-title:Mineralium Deposita
language:en
Short-container-title:Miner Deposita

Author:

Wang Yunfeng,Chen Huayong^ORCID,Baker Michael J.,Han Jinsheng,Xiao Bing,Yang Juntao,Jourdan Fred

Funder

Strategic Priority Research Program (B) of Chinese Academy of Sciences

Natural Science Foundation of China Program

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Economic Geology

Link

http://link.springer.com/content/pdf/10.1007/s00126-018-0859-4.pdf

Reference106 articles.

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3. Audétat A, Pettke T, Heinrich CA, Bodnar RJ (2008) The composition of magmatic-hydrothermal fluids in barren and mineralized intrusions. Econ Geol 103:877–908

4. Ballard JR, Michael-Palin J, Williams IS, Campbell IH, Faunes A (2001) Two ages of porphyry intrusion resolved for the super-giant Chuquicamata copper deposit of northern Chile by ELA-ICP-MS and SHRIMP. Geology 29:383–386

5. Becker SP, Fall A, Bodnar RJ (2008) Synthetic fluid inclusions. XVII. PVTX properties of high-salinity H2O-NaCl solution (>30 wt% NaCl): application to fluid inclusions that homogenize by halite disappearance from porphyry copper and other hydrothermal ore deposits. Econ Geol 103:539–554

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