Miocene Subsidence and Surface Uplift of Southernmost Tibet Induced by Indian Subduction Dynamics-Reference-Cited by-同舟云学术

Miocene Subsidence and Surface Uplift of Southernmost Tibet Induced by Indian Subduction Dynamics

Published:2020-10 Issue:10 Volume:21 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Shen T.¹^ORCID,Wang G.¹^ORCID,Replumaz A.²^ORCID,Husson L.²^ORCID,Webb A. A. G.³^ORCID,Bernet M.²,Leloup P. H.⁴^ORCID,Zhang P.¹,Mahéo G.⁴,Zhang K.⁵

Affiliation:

1. School of Earth Sciences, Center for Global Tectonics, and State Key Laboratory of Geological Processes and Mineral Resources China University of Geosciences Wuhan China

2. Institut des Sciences de la Terre, Université Grenoble Alpes, CNRS Grenoble France

3. Division of Earth and Planetary Science and Laboratory for Space Research University of Hong Kong Hong Kong

4. Laboratoire de Géologie de Lyon, CNRS UMR 5570, Université de Lyon 1 Villeurbanne France

5. School of Earth Sciences and State Key Laboratory of Biogeology and Environmental Geology China University of Geosciences Wuhan China

Funder

National Natural Science Foundation of China

China Geological Survey

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GC009078

Reference115 articles.

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4. Structure and metamorphism of a tectonically thickened continental crust: the Yalu Tsangpo suture zone (Tibet)

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