The Formation and Evolution of Uvarovite in UHP Serpentinite and Rodingite and its Constraints on Chromium Mobility in the Oceanic Subduction Zone-Reference-Cited by-同舟云学术

The Formation and Evolution of Uvarovite in UHP Serpentinite and Rodingite and its Constraints on Chromium Mobility in the Oceanic Subduction Zone

Published:2021-10 Issue:5 Volume:95 Page:1456-1471
ISSN:1000-9515
Container-title:Acta Geologica Sinica - English Edition
language:en
Short-container-title:Acta Geologica Sinica ‐ English Edition

Author:

ZHANG Cong¹,SHEN Tingting¹,ZHANG Lifei²,LIN Congcong³,ZHANG Zhongwei¹,Qin Xueqing¹,HU Han²,QIU Tian¹,XIANG Zhenqun⁴,ZHANG Jianxin¹

Affiliation:

1. Key Laboratory of Deep‐Earth Dynamics of the Ministry of Natural Resources, Institute of Geology Chinese Academy of Geological Sciences Beijing 100037 China

2. School of Earth and Space Sciences Peking University Beijing 100871 China

3. Comprehensive Exploration Technology Center Shandong Coal Field Geological Survey and Research Institute Jinan 250104 China

4. Tianjin Center China Geological Survey Tianjin 300170 China

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/1755-6724.14805

Reference78 articles.

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4. Channelized Fluid Flow and Eclogite-facies Metasomatism along the Subduction Shear Zone

5. Platinum-Group Minerals in Podiform Chromitite from the Kamuikotan Zone, Hokkaido, Northern Japan

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