Fluid evolution of the Wushan skarn-dominant copper deposit in the Middle-Lower Yangtze River metallogenic belt, Eastern China-Reference-Cited by-同舟云学术

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Fluid evolution of the Wushan skarn-dominant copper deposit in the Middle-Lower Yangtze River metallogenic belt, Eastern China

Published:2019-09 Issue: Volume:112 Page:103035
ISSN:0169-1368
Container-title:Ore Geology Reviews
language:en
Short-container-title:Ore Geology Reviews

Author:

Wen Chun-Hua,Shao Yong-Jun,Li Bin,Dick Jeffrey M.,Lai Jian-Qing,Huang Ge-Fei,Luo Xiao-Ya

Funder

National Natural Science Foundation of China

China Postdoctoral Science Foundation

Natural Science Foundation of Hunan Province

Nanjing University

Central South University

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology,Geology

Reference60 articles.

1. Fluid saturation and volatile partitioning between melts and hydrous fluids in crustal magmatic systems: the contribution of experimental measurements and solubility models;Baker;Earth Sci. Rev.,2012

2. FLINCOR: A microcomputer program for the reduction and investigation of fluid inclusion data;Brown;Am. Mineral.,1989

3. P-V-T properties of fluids in the system H2O-CO2-NaCl: New graphical presentations and implications for fluid inclusion studies;Brown;Geochim. Cosmochim. Acta,1989

4. The Copper-Iron Belt of the Lower and Middle Yangtze River;Chang,1991

5. The magmatic–hydrothermal transition—evidence from quartz phenocryst textures and endoskarn abundance in Cu–Zn skarns at the Empire Mine, Idaho, USA;Chang;Chem. Geol.,2004

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