Mechanism of deformation around northern Hejin, China, observed by InSAR

Interierometric synthetic aperture radar (InSAR) images reveal deformation around northern Hejin, Shanxi Province. The small baseline subset (SBAS) approach for InSAR-derived deformation indicates that the observed deformation pattern can be characterized by the sum of two phenomena: background subs...

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Main Authors: Ji Lingyun, Liu Liwei, Li Ning, Liu Ruichun, Zhou Cong
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2013-01-01
Series:Geodesy and Geodynamics
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674984715302226
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spelling doaj-de5010d3683e452398f80761eaf4525c2021-02-02T02:24:36ZengKeAi Communications Co., Ltd.Geodesy and Geodynamics1674-98472013-01-0144414510.3724/SP.J.1246.2013.04041Mechanism of deformation around northern Hejin, China, observed by InSARJi Lingyun0Liu Liwei1Li Ning2Liu Ruichun3Zhou Cong4Second Crust Monitoring and Application Center, China Earthquake Administration, Xi’ an 710054, ChinaSecond Crust Monitoring and Application Center, China Earthquake Administration, Xi’ an 710054, ChinaSecond Crust Monitoring and Application Center, China Earthquake Administration, Xi’ an 710054, ChinaEarthquake Administration of Shanxi Province, China Earthquake Administration, Taiyuan 030021, ChinaSecond Crust Monitoring and Application Center, China Earthquake Administration, Xi’ an 710054, ChinaInterierometric synthetic aperture radar (InSAR) images reveal deformation around northern Hejin, Shanxi Province. The small baseline subset (SBAS) approach for InSAR-derived deformation indicates that the observed deformation pattern can be characterized by the sum of two phenomena: background subsidence from December 2003 to February 2009 with a cumulative displacement of approximately 5 cm and uplift from February 2009 to November 2010 with a cumulative displacement of approximately 2. 5 cm. Deformation modeling indicates that the local deformation was caused by the closing and opening of a sill beneath northern Hejin. The modeled sill which is approximately 5 km long, 2 km wide, is centered at 1. 5 km depth. The deformation was caused by the withdrawal and influx of subsurface water.http://www.sciencedirect.com/science/article/pii/S1674984715302226deformation time seriesnorthern HejinSBAS-InSARdeformation modelingInSAR
collection DOAJ
language English
format Article
sources DOAJ
author Ji Lingyun
Liu Liwei
Li Ning
Liu Ruichun
Zhou Cong
spellingShingle Ji Lingyun
Liu Liwei
Li Ning
Liu Ruichun
Zhou Cong
Mechanism of deformation around northern Hejin, China, observed by InSAR
Geodesy and Geodynamics
deformation time series
northern Hejin
SBAS-InSAR
deformation modeling
InSAR
author_facet Ji Lingyun
Liu Liwei
Li Ning
Liu Ruichun
Zhou Cong
author_sort Ji Lingyun
title Mechanism of deformation around northern Hejin, China, observed by InSAR
title_short Mechanism of deformation around northern Hejin, China, observed by InSAR
title_full Mechanism of deformation around northern Hejin, China, observed by InSAR
title_fullStr Mechanism of deformation around northern Hejin, China, observed by InSAR
title_full_unstemmed Mechanism of deformation around northern Hejin, China, observed by InSAR
title_sort mechanism of deformation around northern hejin, china, observed by insar
publisher KeAi Communications Co., Ltd.
series Geodesy and Geodynamics
issn 1674-9847
publishDate 2013-01-01
description Interierometric synthetic aperture radar (InSAR) images reveal deformation around northern Hejin, Shanxi Province. The small baseline subset (SBAS) approach for InSAR-derived deformation indicates that the observed deformation pattern can be characterized by the sum of two phenomena: background subsidence from December 2003 to February 2009 with a cumulative displacement of approximately 5 cm and uplift from February 2009 to November 2010 with a cumulative displacement of approximately 2. 5 cm. Deformation modeling indicates that the local deformation was caused by the closing and opening of a sill beneath northern Hejin. The modeled sill which is approximately 5 km long, 2 km wide, is centered at 1. 5 km depth. The deformation was caused by the withdrawal and influx of subsurface water.
topic deformation time series
northern Hejin
SBAS-InSAR
deformation modeling
InSAR
url http://www.sciencedirect.com/science/article/pii/S1674984715302226
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AT liuruichun mechanismofdeformationaroundnorthernhejinchinaobservedbyinsar
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