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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Main Authors: Peng Jia, Xi Zhang, Wenquan Zhuang, Fengyun Jiang
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2021-01-01
Series:Geodesy and Geodynamics
Subjects:
GPS
Online Access:http://www.sciencedirect.com/science/article/pii/S1674984721000021
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spelling 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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