Ophiolites in the Xing'an-Inner Mongolia accretionary belt of the CAOB: Implications for two cycles of seafloor spreading and accretionary orogenic events-Reference-Cited by-同舟云学术

Ophiolites in the Xing'an-Inner Mongolia accretionary belt of the CAOB: Implications for two cycles of seafloor spreading and accretionary orogenic events

Published:2015-10 Issue:10 Volume:34 Page:2221-2248
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Song Shuguang¹²,Wang Ming-Ming¹,Xu Xin¹,Wang Chao¹,Niu Yaoling²³,Allen Mark B.²,Su Li⁴

Affiliation:

1. MOE Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences; Peking University; Beijing China

2. Department of Earth Sciences; University of Durham; Durham UK

3. Institute of Oceanology; Chinese Academy of Sciences; Qingdao China

4. Institute of Earth Science; Chinese University of Geosciences; Beijing China

Funder

National Key Basic Research Program of China

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

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