Miocene Volcaniclastic Sequence Within the Xiyu Formation from Source to Sink: Implications for Drainage Development and Tectonic Evolution in Eastern Pamir, NW Tibetan Plateau-Reference-Cited by-同舟云学术

Miocene Volcaniclastic Sequence Within the Xiyu Formation from Source to Sink: Implications for Drainage Development and Tectonic Evolution in Eastern Pamir, NW Tibetan Plateau

Published:2018-09 Issue:9 Volume:37 Page:3261-3284
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Wei Xiaochun¹^ORCID,Zheng Hongbo²,Wang Ping³,Tada Ryuji⁴^ORCID,Clift Peter D.⁵^ORCID,Jourdan Fred⁶^ORCID,Luo Chao³,Chen Hanlin⁷^ORCID

Affiliation:

1. School of Earth Sciences and EngineeringNanjing University Nanjing China

2. Research Center for Earth System ScienceYunnan University Kunming China

3. School of Geography ScienceNanjing Normal University Nanjing China

4. Department of Earth and Planetary ScienceUniversity of Tokyo Tokyo Japan

5. Department of Geology and GeophysicsLouisiana State University Baton Rouge LA USA

6. Western Australian Argon Isotope Facility, Department of Applied Geology and JdL CentreCurtin University Perth WA Australia

7. School of Earth SciencesZhejiang University Hangzhou China

Funder

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018TC005008

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4. Indentation of the Pamirs with respect to the northern margin of Tibet: Constraints from the Tarim basin sedimentary record

5. Linking Tarim Basin sea retreat (west China) and Asian aridification in the late Eocene

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