Late Cretaceous back‐arc extension and arc system evolution in the Gangdese area, southern Tibet: Geochronological, petrological, and Sr‐Nd‐Hf‐O isotopic evidence from Dagze diabases-Reference-Cited by-同舟云学术

Late Cretaceous back‐arc extension and arc system evolution in the Gangdese area, southern Tibet: Geochronological, petrological, and Sr‐Nd‐Hf‐O isotopic evidence from Dagze diabases

Published:2015-09 Issue:9 Volume:120 Page:6159-6181
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Ma Lin¹²,Wang Qiang¹²,Wyman Derek A.³,Jiang Zi‐Qi¹,Wu Fu‐Yuan⁴,Li Xian‐Hua⁴,Yang Jin‐Hui⁴,Gou Guo‐Ning¹,Guo Hai‐Feng¹

Affiliation:

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

2. CAS Center for Excellence in Tibetan Plateau Earth Science Beijing China

3. School of GeosciencesThe University of Sydney Sydney NSW Australia

4. Institute of Geology and GeophysicsChinese Academy of Science Beijing China

Funder

Chinese Academy of Sciences

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015JB011966

Reference152 articles.

1. How deep do common basaltic magmas form and differentiate?

2. Structure and evolution of the Himalaya–Tibet orogenic belt

3. Xigaze forearc basin revisited (South Tibet): Provenance changes and origin of the Xigaze Ophiolite

4. Partition coefficients for olivine-melt and orthopyroxene-melt systems

5. Exhumation of high-pressure rocks driven by slab rollback

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