Disequilibrium partial melting of metasediments in subduction zones: Evidence from O-Nd-Hf isotopes and trace elements in S-type granites of the Chinese Altai-Reference-Cited by-同舟云学术

Disequilibrium partial melting of metasediments in subduction zones: Evidence from O-Nd-Hf isotopes and trace elements in S-type granites of the Chinese Altai

Published:2018-12-20 Issue:1 Volume:11 Page:149-168
ISSN:1941-8264
Container-title:Lithosphere
language:en
Short-container-title:

Author:

Kong Xiangye¹²,Zhang Chen¹³,Liu Dongdong¹²,Jiang Shu⁴,Luo Qun¹²,Zeng Jianhui¹³,Liu Luofu¹³,Luo Long¹,Shao Hengbo¹,Liu Dan²,Liu Xiaoyu¹,Wang Xinpeng¹

Affiliation:

1. State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum Beijing, Beijing 102249, China

2. Unconventional Petroleum Research Institute, China University of Petroleum Beijing, Beijing 102249, China

3. College of Geosciences, China University of Petroleum Beijing, Beijing 102249, China

4. Energy & Geoscience Institute, University of Utah, Salt Lake City, Utah 84108, USA

Publisher

GeoScienceWorld

Subject

Geology

Link

https://pubs.geoscienceworld.org/gsa/lithosphere/article-pdf/11/1/149/4618472/149.pdf

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