Subducted Front of the Indian Continental Crust Beneath the Tibetan Plateau in the Early Eocene-Reference-Cited by-同舟云学术

Subducted Front of the Indian Continental Crust Beneath the Tibetan Plateau in the Early Eocene

Published:2022-09-30 Issue:10 Volume:9 Page:
ISSN:2333-5084
Container-title:Earth and Space Science
language:en
Short-container-title:Earth and Space Science

Author:

Long Xiaoping¹^ORCID,Shu Chutian²,Foley Stephen F.²^ORCID,Wang Xuan‐Ce³,Li Jie⁴^ORCID

Affiliation:

1. State Key Laboratory of Continental Dynamics, Department of Geology Northwest University Xi'an China

2. ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS) ‐ ARC National Key Centre for Geochemical Evolution and Metallogeny of Continents (GEMOC), Department of Earth and Environmental Sciences Macquarie University Sydney NSW Australia

3. Yunnan University Kunming China

4. State Key Laboratory of Isotope Geochemistry Guangzhou Institute of Geochemistry Chinese Academy of Sciences Guangzhou China

Funder

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Environmental Science (miscellaneous)

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022EA002533

Reference74 articles.

1. When and where did India and Asia collide?

2. Osmium isotope binary mixing arrays in arc volcanism

3. Sandstone provenance and tectonic evolution of the Xiukang Mélange from Neotethyan subduction to India–Asia collision (Yarlung-Zangbo suture, south Tibet)

4. Dating the India–Eurasia collision through arc magmatic records

5. The Himalayan passive margin from Precambrian to Cretaceous times

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