Mantle Transition Zone Structure Beneath Northeast Asia From 2‐D Triplicated Waveform Modeling: Implication for a Segmented Stagnant Slab-Reference-Cited by-同舟云学术

Mantle Transition Zone Structure Beneath Northeast Asia From 2‐D Triplicated Waveform Modeling: Implication for a Segmented Stagnant Slab

Author:

Lai Yujing¹²^ORCID,Chen Ling¹²³^ORCID,Wang Tao⁴^ORCID,Zhan Zhongwen⁵^ORCID

Affiliation:

1. State Key Laboratory of Lithospheric Evolution Institute of Geology and Geophysics, Chinese Academy of Sciences Beijing China

2. College of Earth Sciences University of Chinese Academy of Sciences Beijing China

3. CAS Center for Excellence in Tibetan Plateau Earth Sciences Beijing China

4. Institute of Geophysics and Geodynamics, School of Earth Sciences and Engineering Nanjing University Nanjing China

5. Seismological Laboratory California Institute of Technology Pasadena California USA

Funder

National Natural Science Foundation of China

National Science Foundation

CAS-SAFEA International Partnership Program for Creative Research Teams

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

Reference91 articles.

2. Mantle transition zone, stagnant slab and intraplate volcanism in Northeast Asia;Chen C.;Geophysical Journal International,2017

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