4.7 Article

Three-Dimensional Surface Displacements of the 8 January 2022 Mw6.7 Menyuan Earthquake, China from Sentinel-1 and ALOS-2 SAR Observations

期刊

REMOTE SENSING
卷 14, 期 6, 页码 -

出版社

MDPI
DOI: 10.3390/rs14061404

关键词

the 2022 Menyuan earthquake; three-dimensional displacements; InSAR; SM-VCE

资金

  1. National Key Basic Research and Development Program of China [2018YFC1503603]
  2. National Natural Science Foundation of China [42030112]
  3. Nature Science Foundation of Hunan Province [2020JJ2043]
  4. Project of Innovation-Driven Plan of Central South University [2019CX007]
  5. Fundamental Research Funds for the Central Universities of Central South University [2018zzts684, 2019zzts011]
  6. Hunan Provincial Innovation Foundation For Postgraduate [CX20190067]

向作者/读者索取更多资源

This study used SAR data to investigate the surface displacement and strain characteristics of the 2022 Menyuan earthquake, revealing that it was dominated by left-lateral slip and had larger fault-parallel displacement on the southern side. It also identified a severely deformed near-fault area and clearly expanding and compressed zones.
The 8 January 2022 Mw6.7 Menyuan earthquake was generated in the transition zone between the western Lenglongling fault and the eastern Tuolaishan fault, both being part of the Qilian-Haiyuan fault system with an important role in the adjustment of the regional tectonic regime. In this study, four pairs of SAR (synthetic aperture radar) data from Sentinel-1 and ALOS-2 (Advanced Land Observation Satellite-2) satellites were used to derive the surface displacement observations along the satellite line-of-sight (LOS) and azimuth directions using the differential interferometric SAR (InSAR, DInSAR), pixel offset-tracking (POT), multiple aperture InSAR (MAI), and burst overlap InSAR (BOI) methods. An SM-VCE method (i.e., a method for measuring three-dimensional (3D) surface displacements with InSAR based on a strain model and variance component estimation) was employed to combine these derived SAR displacement observations to calculate the 3D co-seismic displacements. Results indicate that the 2022 Menyuan earthquake was dominated by left-lateral slip, and the maximum horizontal and vertical displacements were 1.9 m and 0.6 m, respectively. The relative horizontal surface displacement across the fault was as large as 2-3 m, and the fault-parallel displacement magnitude was larger on the southern side of the fault compared with the northern side. Furthermore, three co-seismic strain invariants were also investigated, revealing that the near-fault area suffered severe deformation, and two obviously expanding and compressed zones were identified. We provide displacements/strains derived in this study in the prevailing geotiff format, which will be useful for the broad community studying this earthquake; in addition, the SM-VCE code used in this study is open to the public so that readers can better understand the method.

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