Horizontal Strain Field in Chinese Mainland and the Surrounding Areas-Reference-Cited by-同舟云学术

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Horizontal Strain Field in Chinese Mainland and the Surrounding Areas

Published:2004-03 Issue:2 Volume:47 Page:245-257
ISSN:0898-9591
Container-title:Chinese Journal of Geophysics
language:en
Short-container-title:Chinese J. Geophys.

Author:

LI Yan-Xing¹,LI Zhi,ZHANG Jing-Hua¹,HUANG Cheng²,ZHU Wen-Yao²,WANG Min³,GUO Liang-Qian¹,ZHANG Zhong-Fu¹,YANG Chun-Hua¹

Affiliation:

1. First Monitoring Center; China Earthquake Administration; Tianjin; 300180; China

2. Shanghai Astronomical Observatory; Chinese Academy of Sciences, Shanghai; 200030; China

3. Center for Analysis and Prediction; China Earthquake Administration; Beijing; 100036; China

Publisher

Wiley

Subject

General Medicine

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/cjg2.480/fullpdf

Reference23 articles.

1. Modern tectonic stress field in the Chinese mainland inversed from focal mechanism solutions;Du;Acta Seismologica Sinica,1999

2. A present-day tectonic stress map for Eastern Asia region;Xu Z;Acta Seismologica Sinica,2001

3. Dynamic mechanism for horizontal deformation in part of North China area;Huang;Acta Seismologica Sinica,1999

4. Research on present crustal deformation in the southern Tianshan (Jiashi) region by GPS geodesy;Wang;Acta Seismologica Sinica,2000

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1. Present-day kinematics and seismic potential of the Ganzi-Yushu fault, eastern Tibetan plateau, constrained from InSAR;Frontiers in Earth Science;2023-01-18

2. Strain-Rates from GPS Measurements in the Ordos Block, China: Implications for Geodynamics and Seismic Hazards;Remote Sensing;2022-02-07

3. Analysis of Crustal Movement and Deformation in Mainland China Based on CMONOC Baseline Time Series;Remote Sensing;2021-06-25

4. Characteristics of block strain and fault movement in the Sichuan-Yunnan region before and after Wenchuan earthquake;Geodesy and Geodynamics;2012-05

5. New Progress in LURR-Integrating with the Dimensional Method;Pure and Applied Geophysics;2012-01-31

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