Interaction of the Indian and Asian Plates Under the Pamir and Hindu‐Kush Regions: Insights From 3‐D Shear Wave Velocity and Anisotropic Structures-Reference-Cited by-同舟云学术

Interaction of the Indian and Asian Plates Under the Pamir and Hindu‐Kush Regions: Insights From 3‐D Shear Wave Velocity and Anisotropic Structures

Published:2020-08 Issue:8 Volume:21 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Liang Yanling¹^ORCID,Li Lun¹²³^ORCID,Liao Jie¹³,Gao Rui¹³^ORCID

Affiliation:

1. School of Earth Sciences and Engineering Sun Yat‐sen University Guangzhou China

2. Guangdong Provincial Key Lab of Geodynamics and Geohazards Guangzhou China

3. Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) Zhuhai China

Funder

Fundamental Research Funds for the Central Universities

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GC009041

Reference66 articles.

1. Seismic Anisotropy in the Earth

2. Cenozoic crustal shortening between the Pamir and Tien Shan and a reconstruction of the Pamir–Tien Shan transition zone for the Cretaceous and Palaeogene

3. Burtman V. S. &Molnar P. H.(1993).Geological and geophysical evidence for deep subduction of continental crust beneath the Pamir(Vol. 281). Geological Society of America.

4. Late Cenozoic slip on the Talas-Ferghana fault, the Tien Shan, central Asia

5. Radial anisotropy in the crust and upper mantle beneath the Qinghai-Tibet Plateau and surrounding regions

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