Regional crustal deformation characteristic before 2016 Yuncheng M4.4 earthquake swarm based on CMONOC continuous GPS data

To further study regional deformation characteristic in the southeast margin of Ordos Block during the period between the Alanshan M5.8 and Yuncheng M4.4 earthquake swarm, we analyze continuous GPS sites around the study area. The time-varying strain parameters removed a linear trend deviated from t...

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Main Authors: Ruichun Liu, Hongwei Li, Shunda Yang
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2016-11-01
Series:Geodesy and Geodynamics
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674984716301550
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spelling doaj-a9edbc7b7d634e34b87e56b38ed376b82021-04-02T10:55:24ZengKeAi Communications Co., Ltd.Geodesy and Geodynamics1674-98472016-11-017645946410.1016/j.geog.2016.09.006Regional crustal deformation characteristic before 2016 Yuncheng M4.4 earthquake swarm based on CMONOC continuous GPS dataRuichun Liu0Hongwei Li1Shunda Yang2Earthquake Administration of Shanxi Province, Taiyuan 030021, ChinaEarthquake Administration of Shanxi Province, Taiyuan 030021, ChinaWutai Earthquake Science and Technology Center, Xinzhou 034000, ChinaTo further study regional deformation characteristic in the southeast margin of Ordos Block during the period between the Alanshan M5.8 and Yuncheng M4.4 earthquake swarm, we analyze continuous GPS sites around the study area. The time-varying strain parameters removed a linear trend deviated from the background state in varying degrees since April, 2015, and began to turn back at the end of the year 2015, meanwhile, the maximum extension strain and shear strain have the bigger variation relative to others. The GPS measurement also shows that the eastward displacement rate of the stations decreases during 2015–2016 in varying degrees compared to 2011–2015, and the variation is closely related to its geologic structural location. The differential movement between the stations is converted into regional strain accumulation due to the fault locking. Furthermore, during 2015–2016, the maximum extension rate oriented at near NS direction obviously increased, and the maximum contraction strain direction is changed from NW to EW direction, which contributes to strengthen extension and shear strain of the NE-striking faults, it's consistent with the regional background strain state of Shanxi seismic zone, this may be an important contributor to occurrence of M4.4 earthquake swarm in Yuncheng basin.http://www.sciencedirect.com/science/article/pii/S1674984716301550Yuncheng M4.4 earthquake swarmTime-varying strainRobust least squares fitRegional deformation characteristic
collection DOAJ
language English
format Article
sources DOAJ
author Ruichun Liu
Hongwei Li
Shunda Yang
spellingShingle Ruichun Liu
Hongwei Li
Shunda Yang
Regional crustal deformation characteristic before 2016 Yuncheng M4.4 earthquake swarm based on CMONOC continuous GPS data
Geodesy and Geodynamics
Yuncheng M4.4 earthquake swarm
Time-varying strain
Robust least squares fit
Regional deformation characteristic
author_facet Ruichun Liu
Hongwei Li
Shunda Yang
author_sort Ruichun Liu
title Regional crustal deformation characteristic before 2016 Yuncheng M4.4 earthquake swarm based on CMONOC continuous GPS data
title_short Regional crustal deformation characteristic before 2016 Yuncheng M4.4 earthquake swarm based on CMONOC continuous GPS data
title_full Regional crustal deformation characteristic before 2016 Yuncheng M4.4 earthquake swarm based on CMONOC continuous GPS data
title_fullStr Regional crustal deformation characteristic before 2016 Yuncheng M4.4 earthquake swarm based on CMONOC continuous GPS data
title_full_unstemmed Regional crustal deformation characteristic before 2016 Yuncheng M4.4 earthquake swarm based on CMONOC continuous GPS data
title_sort regional crustal deformation characteristic before 2016 yuncheng m4.4 earthquake swarm based on cmonoc continuous gps data
publisher KeAi Communications Co., Ltd.
series Geodesy and Geodynamics
issn 1674-9847
publishDate 2016-11-01
description To further study regional deformation characteristic in the southeast margin of Ordos Block during the period between the Alanshan M5.8 and Yuncheng M4.4 earthquake swarm, we analyze continuous GPS sites around the study area. The time-varying strain parameters removed a linear trend deviated from the background state in varying degrees since April, 2015, and began to turn back at the end of the year 2015, meanwhile, the maximum extension strain and shear strain have the bigger variation relative to others. The GPS measurement also shows that the eastward displacement rate of the stations decreases during 2015–2016 in varying degrees compared to 2011–2015, and the variation is closely related to its geologic structural location. The differential movement between the stations is converted into regional strain accumulation due to the fault locking. Furthermore, during 2015–2016, the maximum extension rate oriented at near NS direction obviously increased, and the maximum contraction strain direction is changed from NW to EW direction, which contributes to strengthen extension and shear strain of the NE-striking faults, it's consistent with the regional background strain state of Shanxi seismic zone, this may be an important contributor to occurrence of M4.4 earthquake swarm in Yuncheng basin.
topic Yuncheng M4.4 earthquake swarm
Time-varying strain
Robust least squares fit
Regional deformation characteristic
url http://www.sciencedirect.com/science/article/pii/S1674984716301550
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AT hongweili regionalcrustaldeformationcharacteristicbefore2016yunchengm44earthquakeswarmbasedoncmonoccontinuousgpsdata
AT shundayang regionalcrustaldeformationcharacteristicbefore2016yunchengm44earthquakeswarmbasedoncmonoccontinuousgpsdata
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