Multiple mineralization events at Paleozoic Sanchakou porphyry Cu deposit, Xinjiang: New insights from geology, geochronology, fluid inclusions, and H-O-C isotopes-Reference-Cited by-同舟云学术

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Multiple mineralization events at Paleozoic Sanchakou porphyry Cu deposit, Xinjiang: New insights from geology, geochronology, fluid inclusions, and H-O-C isotopes

Published:2023-12 Issue: Volume:163 Page:105726
ISSN:0169-1368
Container-title:Ore Geology Reviews
language:en
Short-container-title:Ore Geology Reviews

Author:

Zhang Fang-Fang,Wang Yin-Hong,Liu Jia-Jun,Zhang Zhong-Yu,Wang Jian-Ping,Geng Rui-Rui,Zhang Wei,Du Xiao-Wei

Funder

Higher Education Discipline Innovation Project

Fundamental Research Funds for the Central Universities

National Natural Science Foundation of China

Ministry of Science and Technology of the People's Republic of China

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology,Geology

Reference88 articles.

1. Thermochemical data of pure substances;Barin,1989

2. Calculation of fractionation factors for carbon and oxygen isotopic exchange in the system calcite-carbon dioxide-water;Bottinga;J. Phys. Chem.,1968

3. Diffusion of osmium in pyrrhotite and pyrite: implications for closure of the Re-Os isotopic system;Brenan;Earth Planet Sc. Lett.,2000

4. Ore fluids - magmatic to supergene;Brimhall;Rev. Mineral.,1987

5. Cation site occupancy in chlorites and illites as a function of temperature;Cathelineau;Clay Miner.,1988

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1. Fluid evolution of the Nulasai Cu deposit, Xinjiang, NW China: Evidence from fluid inclusions and O-H-C isotopes;Ore Geology Reviews;2024-10

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