Hydrous juvenile lower crust at the western Yangtze Craton margin as the main source of the Beiya porphyry‐skarn Au deposit-Reference-Cited by-同舟云学术

Hydrous juvenile lower crust at the western Yangtze Craton margin as the main source of the Beiya porphyry‐skarn Au deposit

Published:2021-07-05 Issue: Volume: Page:
ISSN:1000-9515
Container-title:Acta Geologica Sinica - English Edition
language:en
Short-container-title:Acta Geologica Sinica (Eng)

Author:

WANG Zixuan¹,ZHENG Yuanchuan¹,XU Bo²,HOU Zengqian³,ZHANG Aiping⁴,SHEN Yang¹,MA Rui¹,WU Changda³,XU Peiyan¹

Affiliation:

1. State Key Laboratory of Geological Processes and Mineral Resources and School of Earth Sciences and Resources China University of Geosciences Beijing 100083 People's Republic of China

2. School of Gemmology China University of Geosciences Beijing 100083 People's Republic of China

3. Institute of Geology Chinese Academy of Geological Sciences Beijing 100037 People's Republic of China

4. College of Resource Environment and Earth Sciences Yunnan University Kunming 650091 People's Republic of China

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/1755-6724.14788

Reference178 articles.

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3. Absolute18O content of standard mean ocean water

4. Beane R.E. andTitley S.R. 1981.Porphyry copper deposits. Part II. Hydrothermal alteration and mineralization. Economic Geology 75THAnniversary Volume p.235–269.

5. A catalytic delamination-driven model for coupled genesis of Archaean crust and sub-continental lithospheric mantle

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