Mineralogy, Fluid Inclusion, and Hydrogen and Oxygen Isotope Studies of the Intrusion‐Related Yangla Cu Deposit in the Sanjiang Region, SW China: Implications for Metallogenesis and Deposit Type-Reference-Cited by-同舟云学术

Mineralogy, Fluid Inclusion, and Hydrogen and Oxygen Isotope Studies of the Intrusion‐Related Yangla Cu Deposit in the Sanjiang Region, SW China: Implications for Metallogenesis and Deposit Type

Published:2019-09 Issue:1 Volume:70 Page:28-49
ISSN:1344-1698
Container-title:Resource Geology
language:en
Short-container-title:Resource Geology

Author:

Du Li‐Juan¹²^ORCID,Li Bo³,Huang Zhi‐Long²,Chen Jun²,Zhou Jia‐Xi²,Zou Guo‐Fu⁴,Yan Zai‐Fei²

Affiliation:

1. College of Resources and Environmental EngineeringGuizhou University Guiyang China

2. State Key Laboratory of Ore Deposit Geochemistry, Institute of GeochemistryChinese Academy of Sciences Guiyang China

3. Faculty of Land Resources EngineeringKunming University of Science and Technology Kunming China

4. Yunnan Copper GroupKunming Prospecting Design Inst China Nonferrous Kunming China

Funder

National Natural Science Foundation of China

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/rge.12215

Reference92 articles.

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3. Fluid‐inclusion evidence for a magmatic source for metals in porphyry copper deposits;Bodnar R. J.;Mineral. Assoc. Canada Short Course Series,1995

4. Fluid Inclusions in Hydrothermal Ore Deposits

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