In-situ central Qiangtang metamorphic belt in western Tibet as a typical suture zone: Evidence of crust-mantle structural footprints from P-wave receiver function analyses

Author:

Niu Xiao,He Rizheng,Zheng Hongwei,Wu Wei,Ji Zhanbo

Funder

National Natural Science Foundation of China

China Geological Survey

China Earthquake Administration

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference105 articles.

1. On the nonuniqueness of receiver function inversions;Ammon;J. Geophys. Res.,1990

2. Bright spots, structure, and magmatism in southern Tibet from indepth seismic reflection profling;Brown;Science,1996

3. The geological tectonic characteristics of the Qomolangma region in South Tibet of China and the formation of east-west mountain series on the Qinghai-Tibet plateau;Chang;Sci. China,1973

4. Shear-wave birefringence and current configuration of converging lithosphere under Tibet;Chen;Earth Planet. Sci. Lett.,2010

5. Tibetan tectonic evolution inferred from spatial and temporal variations in post-collisional magmatism;Chung;Earth Sci. Rev.,2005

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