GPS observation in Sichuan-Yunnan and its vicinity before and after the Wenchuan earthquake in a decade
Based on the horizontal velocity data observed by GPS during 2004–2007, 2007–2009, and 2011–2017 before, during, and after the Wenchuan earthquake in Sichuan-Yunnan and its vicinity, we analyze evolution features of the tectonic deformation caused by crustal movement in main active fault belts, and...
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KeAi Communications Co., Ltd.
2021-01-01
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Online Access: | http://www.sciencedirect.com/science/article/pii/S1674984721000021 |
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doaj-f36c8a3f143f4a7599575f9f75ab34002021-03-17T04:13:57ZengKeAi Communications Co., Ltd.Geodesy and Geodynamics1674-98472021-01-011214347GPS observation in Sichuan-Yunnan and its vicinity before and after the Wenchuan earthquake in a decadePeng Jia0Xi Zhang1Wenquan Zhuang2Fengyun Jiang3Corresponding author.; Second Monitoring and Application Center, CEA, ChinaSecond Monitoring and Application Center, CEA, ChinaSecond Monitoring and Application Center, CEA, ChinaSecond Monitoring and Application Center, CEA, ChinaBased on the horizontal velocity data observed by GPS during 2004–2007, 2007–2009, and 2011–2017 before, during, and after the Wenchuan earthquake in Sichuan-Yunnan and its vicinity, we analyze evolution features of the tectonic deformation caused by crustal movement in main active fault belts, and its possible influence. We conclude: the Wenchuan earthquake area showed obvious co-seismic thrust and dextral deformation from 2007 to 2009. The earthquake, to a certain extent, promoted tectonic movements on the Gansu-Sichuan boundary, Western Qinling fault zone, Anninghe-Zemuhe fault zone, and southern Xianshuihe fault zone. The vectors and strain filed acquired by GPS during Lushan and Jiuzhaigou earthquakes period may indicate that the southwest segment in the Longmenshan fault zone still has the possibility of larger earthquakes.http://www.sciencedirect.com/science/article/pii/S1674984721000021Sichuan-Yunnan and its vicinityThe Wenchuan earthquakeGPSTectonic deformationJiuzhaigou |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Peng Jia Xi Zhang Wenquan Zhuang Fengyun Jiang |
spellingShingle |
Peng Jia Xi Zhang Wenquan Zhuang Fengyun Jiang GPS observation in Sichuan-Yunnan and its vicinity before and after the Wenchuan earthquake in a decade Geodesy and Geodynamics Sichuan-Yunnan and its vicinity The Wenchuan earthquake GPS Tectonic deformation Jiuzhaigou |
author_facet |
Peng Jia Xi Zhang Wenquan Zhuang Fengyun Jiang |
author_sort |
Peng Jia |
title |
GPS observation in Sichuan-Yunnan and its vicinity before and after the Wenchuan earthquake in a decade |
title_short |
GPS observation in Sichuan-Yunnan and its vicinity before and after the Wenchuan earthquake in a decade |
title_full |
GPS observation in Sichuan-Yunnan and its vicinity before and after the Wenchuan earthquake in a decade |
title_fullStr |
GPS observation in Sichuan-Yunnan and its vicinity before and after the Wenchuan earthquake in a decade |
title_full_unstemmed |
GPS observation in Sichuan-Yunnan and its vicinity before and after the Wenchuan earthquake in a decade |
title_sort |
gps observation in sichuan-yunnan and its vicinity before and after the wenchuan earthquake in a decade |
publisher |
KeAi Communications Co., Ltd. |
series |
Geodesy and Geodynamics |
issn |
1674-9847 |
publishDate |
2021-01-01 |
description |
Based on the horizontal velocity data observed by GPS during 2004–2007, 2007–2009, and 2011–2017 before, during, and after the Wenchuan earthquake in Sichuan-Yunnan and its vicinity, we analyze evolution features of the tectonic deformation caused by crustal movement in main active fault belts, and its possible influence. We conclude: the Wenchuan earthquake area showed obvious co-seismic thrust and dextral deformation from 2007 to 2009. The earthquake, to a certain extent, promoted tectonic movements on the Gansu-Sichuan boundary, Western Qinling fault zone, Anninghe-Zemuhe fault zone, and southern Xianshuihe fault zone. The vectors and strain filed acquired by GPS during Lushan and Jiuzhaigou earthquakes period may indicate that the southwest segment in the Longmenshan fault zone still has the possibility of larger earthquakes. |
topic |
Sichuan-Yunnan and its vicinity The Wenchuan earthquake GPS Tectonic deformation Jiuzhaigou |
url |
http://www.sciencedirect.com/science/article/pii/S1674984721000021 |
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