Large-Scale Crustal Deformation of the Tianshan Mountains, Xinjiang, from Sentinel-1 InSAR Observations (2015–2020)

In this paper, we address some questions with respect to the Tianshan Mountains that are necessary for understanding the present deformation rate in this region. A series of thrust nappe structures are distributed on the north and south sides of the Tianshan Mountains, and many of them are currently...

Full description

Bibliographic Details
Main Authors: Pengcheng Sha, Xiufeng He, Xiaohang Wang, Zhuang Gao
Format: Article
Language:English
Published: MDPI AG 2023-10-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/15/20/4901
_version_ 1797572406331572224
author Pengcheng Sha
Xiufeng He
Xiaohang Wang
Zhuang Gao
author_facet Pengcheng Sha
Xiufeng He
Xiaohang Wang
Zhuang Gao
author_sort Pengcheng Sha
collection DOAJ
description In this paper, we address some questions with respect to the Tianshan Mountains that are necessary for understanding the present deformation rate in this region. A series of thrust nappe structures are distributed on the north and south sides of the Tianshan Mountains, and many of them are currently active. To analyze the deformation characteristics and movement rates of different fold-and-thrust belts on the northern and southern margins of Tianshan, we use InSAR observations (Sentinel-1A/B, 2015–2020) to produce a rate map for the entire observation period on four ascending and four descending tracks. In order to reduce phase artifacts, we reconstruct multi-temporal scenes with atmospheric-corrected and orbital-corrected interferograms via a small baseline subset. The results show that the Bolokenu-Aqikekuduke Fault exhibits a right-lateral strike-slip motion, with the western segment moving at about 4.95 ± 0.38 mm/yr and the eastern segment at approximately 2.34 ± 0.34 mm/yr. The Manas-Tugulu anticline in the northern fold-and-thrust belt reaches ~5–8 mm/yr at 86°E–86.5°, and the Qiulitage anticline in the south reaches ~6–9 mm/yr at ~83°–85°. The post-seismic time series cumulative displacement map of the Jinghe earthquake reveals no significant post-seismic deformation signal in the epicenter area. The Qiulitage thrust belt, situated within the fold-and-thrust belts flanking the Tianshan, features extensive thrust accompanied by a right-lateral strike-slip component. And the Manas-Tugulu anticline exhibits sustained deformation, including pronounced coseismic and post-seismic effects from the Hutubi earthquake. This study highlights the potential of a multi-temporal InSAR analysis and emphasizes future opportunities presented by new generations of SAR platforms with shorter revisit periods for quantifying the spatial and temporal behavior of post-seismic and interseismic periods.
first_indexed 2024-03-10T20:55:49Z
format Article
id doaj.art-8f5b714979ea4ff6b9ec9c1203c4a97e
institution Directory Open Access Journal
issn 2072-4292
language English
last_indexed 2024-03-10T20:55:49Z
publishDate 2023-10-01
publisher MDPI AG
record_format Article
series Remote Sensing
spelling doaj.art-8f5b714979ea4ff6b9ec9c1203c4a97e2023-11-19T17:58:01ZengMDPI AGRemote Sensing2072-42922023-10-011520490110.3390/rs15204901Large-Scale Crustal Deformation of the Tianshan Mountains, Xinjiang, from Sentinel-1 InSAR Observations (2015–2020)Pengcheng Sha0Xiufeng He1Xiaohang Wang2Zhuang Gao3School of Earth Sciences and Engineering, Hohai University, Nanjing 211100, ChinaSchool of Earth Sciences and Engineering, Hohai University, Nanjing 211100, ChinaSchool of Geodesy and Geomatics, Wuhan University, 129 Luoyu Road, Wuhan 430079, ChinaSchool of Earth Sciences and Engineering, Hohai University, Nanjing 211100, ChinaIn this paper, we address some questions with respect to the Tianshan Mountains that are necessary for understanding the present deformation rate in this region. A series of thrust nappe structures are distributed on the north and south sides of the Tianshan Mountains, and many of them are currently active. To analyze the deformation characteristics and movement rates of different fold-and-thrust belts on the northern and southern margins of Tianshan, we use InSAR observations (Sentinel-1A/B, 2015–2020) to produce a rate map for the entire observation period on four ascending and four descending tracks. In order to reduce phase artifacts, we reconstruct multi-temporal scenes with atmospheric-corrected and orbital-corrected interferograms via a small baseline subset. The results show that the Bolokenu-Aqikekuduke Fault exhibits a right-lateral strike-slip motion, with the western segment moving at about 4.95 ± 0.38 mm/yr and the eastern segment at approximately 2.34 ± 0.34 mm/yr. The Manas-Tugulu anticline in the northern fold-and-thrust belt reaches ~5–8 mm/yr at 86°E–86.5°, and the Qiulitage anticline in the south reaches ~6–9 mm/yr at ~83°–85°. The post-seismic time series cumulative displacement map of the Jinghe earthquake reveals no significant post-seismic deformation signal in the epicenter area. The Qiulitage thrust belt, situated within the fold-and-thrust belts flanking the Tianshan, features extensive thrust accompanied by a right-lateral strike-slip component. And the Manas-Tugulu anticline exhibits sustained deformation, including pronounced coseismic and post-seismic effects from the Hutubi earthquake. This study highlights the potential of a multi-temporal InSAR analysis and emphasizes future opportunities presented by new generations of SAR platforms with shorter revisit periods for quantifying the spatial and temporal behavior of post-seismic and interseismic periods.https://www.mdpi.com/2072-4292/15/20/4901InSARTianshan MountainBolokenu-Aqikekuduke FaultManas thrust-and-foldJinghe earthquakeSentinel-1 satellite
spellingShingle Pengcheng Sha
Xiufeng He
Xiaohang Wang
Zhuang Gao
Large-Scale Crustal Deformation of the Tianshan Mountains, Xinjiang, from Sentinel-1 InSAR Observations (2015–2020)
Remote Sensing
InSAR
Tianshan Mountain
Bolokenu-Aqikekuduke Fault
Manas thrust-and-fold
Jinghe earthquake
Sentinel-1 satellite
title Large-Scale Crustal Deformation of the Tianshan Mountains, Xinjiang, from Sentinel-1 InSAR Observations (2015–2020)
title_full Large-Scale Crustal Deformation of the Tianshan Mountains, Xinjiang, from Sentinel-1 InSAR Observations (2015–2020)
title_fullStr Large-Scale Crustal Deformation of the Tianshan Mountains, Xinjiang, from Sentinel-1 InSAR Observations (2015–2020)
title_full_unstemmed Large-Scale Crustal Deformation of the Tianshan Mountains, Xinjiang, from Sentinel-1 InSAR Observations (2015–2020)
title_short Large-Scale Crustal Deformation of the Tianshan Mountains, Xinjiang, from Sentinel-1 InSAR Observations (2015–2020)
title_sort large scale crustal deformation of the tianshan mountains xinjiang from sentinel 1 insar observations 2015 2020
topic InSAR
Tianshan Mountain
Bolokenu-Aqikekuduke Fault
Manas thrust-and-fold
Jinghe earthquake
Sentinel-1 satellite
url https://www.mdpi.com/2072-4292/15/20/4901
work_keys_str_mv AT pengchengsha largescalecrustaldeformationofthetianshanmountainsxinjiangfromsentinel1insarobservations20152020
AT xiufenghe largescalecrustaldeformationofthetianshanmountainsxinjiangfromsentinel1insarobservations20152020
AT xiaohangwang largescalecrustaldeformationofthetianshanmountainsxinjiangfromsentinel1insarobservations20152020
AT zhuanggao largescalecrustaldeformationofthetianshanmountainsxinjiangfromsentinel1insarobservations20152020