Investigation of the Moho discontinuity beneath the Chinese mainland using deep seismic sounding profiles-Reference-Cited by-同舟云学术

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Investigation of the Moho discontinuity beneath the Chinese mainland using deep seismic sounding profiles

Published:2013-12 Issue: Volume:609 Page:202-216
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Teng Jiwen,Zhang Zhongjie,Zhang Xiankang,Wang Chunyong,Gao Rui,Yang Baojun,Qiao Yonghu,Deng Yangfan

Funder

Ministry of Science and Technology of China

Chinese Academy of Sciences

Chinese National Nature Sciences Foundation

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference238 articles.

1. The crust and upper mantle discontinuity structure beneath Alaska inferred from receiver functions;Ai;Physics of the Earth and Planetary Interiors,2005

2. INDEPTH multichannel seismic reflection data: description and availability;Alsdorf;Journal of Geophysical Research,1988

3. An attempt at 3-D imaging of a small domain (Almeria, southern Spain) using a POCS algorithm;Badal;Physics of the Earth and Planetary Interiors,2000

4. Tomography research of the Zhefang–Binchuan and Menglian–Malong wide-angle seismic profiles in Yunnan province;Bai;Chinese Journal of Geophysics,2004

5. Crustal P-wave velocity structure in the lower Yangtze region: reinterpretation of the Fuliji–Fengxian deep seismic sounding profile;Bai;Chinese Science Bulletin,2006

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1. Crustal and uppermost mantle structure of the northeastern Qinghai-Xizang Plateau from joint inversion of surface wave dispersions and receiver functions with P velocity constraints;Earthquake Science;2024-04

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