Present-day tectonic activity along the central section of the Altyn Tagh fault derived from time series InSAR
The Altyn Tagh Fault (ATF) is a large-scale complex tectonic system. In this study, the present-day crustal deformation of the central section of the ATF (90.8°E−91.58°E) was obtained using 14 images on a descending track acquired between 2007 and 2010 from Advanced Land Observing Satellite (ALOS)....
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Published in | Geodesy and Geodynamics Vol. 10; no. 4; pp. 307 - 314 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
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Elsevier B.V
01.07.2019
KeAi Communications Co., Ltd |
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Abstract | The Altyn Tagh Fault (ATF) is a large-scale complex tectonic system. In this study, the present-day crustal deformation of the central section of the ATF (90.8°E−91.58°E) was obtained using 14 images on a descending track acquired between 2007 and 2010 from Advanced Land Observing Satellite (ALOS). To improve the accuracy of the interferograms, ALOS World 3D–30m (AW3D-30)Digital Surface Model (DSM) from the Japan Aerospace Exploration Agency was used in Small Baseline Subset (SBAS) Interferometric Synthetic Aperture Radar (InSAR) processing. The Line of Sight (LOS) deformation map show that there is an obvious zoning feature. With the main ATF as the boundary, the north block is concentrated around −35∼ −60 mm, and the south block is concentrated around −9 ∼ 11 mm. Based on the InSAR velocity map, we inverted for the strike-slip rate and locking depth of the fault using the two-dimensional strike-slip fault buried-dislocation model. The inversion results for the strike-slip rate at three selected cross-section locations perpendicular to the ATF were 6.1 mm/a, 5.3 mm/a and 7.9 mm/a from west to east; the corresponding locking depths were 9.5 km, 6.8 km and 12.3 km from west to east. The location and trend of the fault obtained by inversion are coincides with the Xorkol seismic belt. |
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AbstractList | The Altyn Tagh Fault (ATF) is a large-scale complex tectonic system. In this study, the present-day crustal deformation of the central section of the ATF (90.8°E−91.58°E) was obtained using 14 images on a descending track acquired between 2007 and 2010 from Advanced Land Observing Satellite (ALOS). To improve the accuracy of the interferograms, ALOS World 3D–30m (AW3D-30)Digital Surface Model (DSM) from the Japan Aerospace Exploration Agency was used in Small Baseline Subset (SBAS) Interferometric Synthetic Aperture Radar (InSAR) processing. The Line of Sight (LOS) deformation map show that there is an obvious zoning feature. With the main ATF as the boundary, the north block is concentrated around −35∼ −60 mm, and the south block is concentrated around −9 ∼ 11 mm. Based on the InSAR velocity map, we inverted for the strike-slip rate and locking depth of the fault using the two-dimensional strike-slip fault buried-dislocation model. The inversion results for the strike-slip rate at three selected cross-section locations perpendicular to the ATF were 6.1 mm/a, 5.3 mm/a and 7.9 mm/a from west to east; the corresponding locking depths were 9.5 km, 6.8 km and 12.3 km from west to east. The location and trend of the fault obtained by inversion are coincides with the Xorkol seismic belt. The Altyn Tagh Fault (ATF) is a large-scale complex tectonic system. In this study, the present-day crustal deformation of the central section of the ATF (90.8°E−91.58°E) was obtained using 14 images on a descending track acquired between 2007 and 2010 from Advanced Land Observing Satellite (ALOS). To improve the accuracy of the interferograms, ALOS World 3D–30m (AW3D-30)Digital Surface Model (DSM) from the Japan Aerospace Exploration Agency was used in Small Baseline Subset (SBAS) Interferometric Synthetic Aperture Radar (InSAR) processing. The Line of Sight (LOS) deformation map show that there is an obvious zoning feature. With the main ATF as the boundary, the north block is concentrated around −35∼ −60 mm, and the south block is concentrated around −9 ∼ 11 mm. Based on the InSAR velocity map, we inverted for the strike-slip rate and locking depth of the fault using the two-dimensional strike-slip fault buried-dislocation model. The inversion results for the strike-slip rate at three selected cross-section locations perpendicular to the ATF were 6.1 mm/a, 5.3 mm/a and 7.9 mm/a from west to east; the corresponding locking depths were 9.5 km, 6.8 km and 12.3 km from west to east. The location and trend of the fault obtained by inversion are coincides with the Xorkol seismic belt. Keywords: InSAR, Altyn Tagh Fault system, Strike-slip rate, Geodetic inversion |
Author | Wang, Yang Wang, Chen Qiu, Jiangtao Liu, Lei |
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CitedBy_id | crossref_primary_10_1016_j_jseaes_2022_105082 crossref_primary_10_3390_rs12203362 crossref_primary_10_1007_s00024_021_02735_w crossref_primary_10_1007_s10950_020_09930_7 crossref_primary_10_1088_1755_1315_1276_1_012022 crossref_primary_10_1109_JSTARS_2023_3318053 crossref_primary_10_1016_j_jvolgeores_2021_107272 |
Cites_doi | 10.1002/2017JB014465 10.1109/LGRS.2011.2156381 10.1002/2013GL057497 10.1029/2005JB004120 10.1029/2012JB009289 10.3390/rs8030233 10.1109/TGRS.2002.803792 10.1029/2008GL033659 10.1029/2004JB003210 10.1029/2005JB004014 10.1109/TGRS.2010.2043739 10.1029/JB078i005p00832 |
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Keywords | Altyn Tagh Fault system InSAR Strike-slip rate Geodetic inversion |
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Snippet | The Altyn Tagh Fault (ATF) is a large-scale complex tectonic system. In this study, the present-day crustal deformation of the central section of the ATF... |
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SubjectTerms | Altyn Tagh Fault system Geodetic inversion InSAR Strike-slip rate |
Title | Present-day tectonic activity along the central section of the Altyn Tagh fault derived from time series InSAR |
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