Fluid Evolution and Ore-forming Processes of the Jiama Cu Deposit, Tibet: Evidence from Fluid Inclusions

Author:

YAO Xiaofeng12,LIU Jiajun1,TANG Juxing3,ZHENG Wenbao3,ZHANG Zhi4

Affiliation:

1. China University of Geosciences; Beijing 100083 China

2. Development and Research Center; China Geological Survey (CGS); Beijing 100037 China

3. Key Laboratory of Metallogeny and Mineral Resources Assessment MLR, Institute of Mineral Resources; Chinese Academy of Geological Sciences (CAGS); Beijing 100037 China

4. Chengdu Institute of Geology and Mineral Resources; China Geological Survey; Chengdu 610082 Sichuan China

Publisher

Wiley

Subject

Geology

Reference68 articles.

1. Composition and evolution of ore fluids in a magmatic-hydrothermal skarn deposit;Baker;Geology,2004

2. Magmas and hydrothermal fluids;Burnham,1979

3. Mineralization, alteration, and structural evolution of the El Teniente porphyry Cu-Mo deposit;Cannell;Economic Geology,2005

4. Validation and representation of fluid inclusion microthermometric data using the fluid inclusion assemblage (FIA) concept;Guoxiang;Acta Petrologica Sinica,2008

5. Constraints from fluid inclusion studies on hydrodynamic models of mineralization;Guoxiang;Acta Petrologica Sinica,2015

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