Lateral Variations of Shear‐Wave Velocity in the D″ Layer Beneath the Indian‐Eurasian Plate Collision Zone-Reference-Cited by-同舟云学术

Lateral Variations of Shear‐Wave Velocity in the D″ Layer Beneath the Indian‐Eurasian Plate Collision Zone

Published:2020-03-20 Issue:6 Volume:47 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Li Guohui¹²^ORCID,Bai Ling¹^ORCID,Ritsema Jeroen³^ORCID

Affiliation:

1. Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, Center for Excellence in Tibetan Plateau Earth Sciences Chinese Academy of Sciences Beijing China

2. Institute of Earthquake Forecasting China Earthquake Administration Beijing China

3. Department of Earth and Environmental Sciences University of Michigan Ann Arbor MI USA

Funder

China Postdoctoral Science Foundation

National Natural Science Foundation of China

National Science Foundation

K. C. Wong Education Foundation

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL086856

Reference50 articles.

1. Melting of subducted basalt at the core-mantle boundary

2. Focal depths and mechanisms of shallow earthquakes in the Himalayan–Tibetan region

3. Iron–silica interaction at extreme conditions and the electrically conducting layer at the base of Earth's mantle

4. A strong lateral shear velocity gradient and anisotropy heterogeneity in the lowermost mantle beneath the southern Pacific

5. Investigation of laterally heterogeneous shear velocity structure in D″ beneath Eurasia

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