Cenozoic crustal-scale duplexing and flat Moho in southern Tibet: Evidence from reflection seismology-Reference-Cited by-同舟云学术

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Cenozoic crustal-scale duplexing and flat Moho in southern Tibet: Evidence from reflection seismology

Published:2020-09 Issue: Volume:790 Page:228562
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Shi Zhuoxuan^ORCID,Gao Rui,Li Wenhui,Lu Zhanwu,Li Hongqiang

Funder

National Key R&D Program of China

National Natural Science Foundation of China

Chinese Geological Survey project

Pearl River Talent Recruitment Program

Fund from the Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference57 articles.

1. Himalayan tectonics explained by extrusion of a low-viscosity crustal channel coupled to focused surface denudation;Beaumont;Nature,2002

2. Lateral extrusion of lower crust from under high topography in the isostatic limit;Bird;J. Geophys. Res.,1991

3. Strong attenuation of Rayleigh waves in Tibet;Bird;Nature,1977

4. A “no-lid” zone in the central Chang-Thang platform of Tibet: evidence from pure path phase velocity measurements of long period Rayleigh waves;Brandon;J. Geophys. Res,1986

5. COCORP: new perspectives on the deep crust;Brown;Geophys J. Int.,1987

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