Postcollisional delamination and partial melting of enriched lithospheric mantle: Evidence from Oligocene (ca. 30 Ma) potassium-rich lavas in the Gemuchaka area of the central Qiangtang Block, Tibet-Reference-Cited by-同舟云学术

Postcollisional delamination and partial melting of enriched lithospheric mantle: Evidence from Oligocene (ca. 30 Ma) potassium-rich lavas in the Gemuchaka area of the central Qiangtang Block, Tibet

Published:2018-12-05 Issue:7-8 Volume:131 Page:1385-1408
ISSN:0016-7606
Container-title:GSA Bulletin
language:en
Short-container-title:

Author:

Ou Quan¹²,Wang Qiang¹³⁴,Wyman Derek A.⁵,Zhang Chunfu⁶,Hao Lu-Lu¹,Dan Wei¹,Jiang Zi-Qi¹⁷,Wu Fu-Yuan⁸,Yang Jin-Hui⁸,Zhang Hai-Xiang¹,Xia Xiao-Ping¹,Ma Lin¹,Long Xiao-Ping¹,Li Jie¹

Affiliation:

1. State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China

2. Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, School of Geosciences and Info-Physics, Central South University, Changsha 410083, China

3. CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing 100101, China

4. College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China

5. School of Geosciences, The University of Sydney, New South Wales 2006, Australia

6. Department of Geosciences, Fort Hays State University, Hays, Kansas 67601-4099, USA

7. School of Earth Science, Guilin University of Technology, Guilin 541004, China

8. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

Publisher

Geological Society of America

Subject

Geology

Link

https://pubs.geoscienceworld.org/gsa/gsabulletin/article-pdf/131/7-8/1385/4729868/1385.pdf

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