Hydrothermal evolution and ore precipitation of the No. 2 porphyry Cu–Au deposit in the Xiongcun district, Tibet: Evidence from cathodoluminescence, fluid inclusions, and isotopes-Reference-Cited by-同舟云学术

Hydrothermal evolution and ore precipitation of the No. 2 porphyry Cu–Au deposit in the Xiongcun district, Tibet: Evidence from cathodoluminescence, fluid inclusions, and isotopes

Published:2019-11 Issue: Volume:114 Page:103141
ISSN:0169-1368
Container-title:Ore Geology Reviews
language:en
Short-container-title:Ore Geology Reviews

Author:

Lang Xinghai,Wang Xuhui^ORCID,Deng Yulin,Tang Juxing,Xie Fuwei,Yang Zongyao,Yin Qing,Jiang Kai

Funder

Deep Resources Exploration and Mining, the National Key R&D Program of China

National Natural Science Foundation of China

Opening Foundation of State Key Laboratory for Mineral Deposits Research

Opening Foundation of State Key Laboratory of Continental Dynamics, Northwest University

Opening Foundation of State Key Laboratory of Ore Deposit Geochemistry

China Geological Survey Programs

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology,Geology

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5. Interpretation of microthermometric data for H2O-NaCl fluid inclusions;Bodnar,1994

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