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2022 Vol. 28, No. 6
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ZHAO Chaoying, LIU Xiaojie, GAO Yang, FENG Xiaosong. 2022. Early identification of high-elevation geohazards in the lower Yarlung Zangbo River based on the SAR/InSAR technology. Journal of Geomechanics, 28(6): 981-994. doi: 10.12090/j.issn.1006-6616.20222825
Citation: ZHAO Chaoying, LIU Xiaojie, GAO Yang, FENG Xiaosong. 2022. Early identification of high-elevation geohazards in the lower Yarlung Zangbo River based on the SAR/InSAR technology. Journal of Geomechanics, 28(6): 981-994. doi: 10.12090/j.issn.1006-6616.20222825
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Early identification of high-elevation geohazards in the lower Yarlung Zangbo River based on the SAR/InSAR technology

  • 1.

    School of Geological Engineering and Geomatics, Chang'an University, Xi'an 710054, Shaanxi, China

  • 2.

    Key Laboratory of Western China's Mineral Resources and Geological Engineering, Ministry of Education, Xi'an 710054, Shaanxi, China

  • 3.

    Key Laboratory of Ecological Geology and Disaster Prevention, Ministry of Natural Resources, Xi'an 710054, Shaanxi, China

  • 4.

    Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

    • Fund Project: This research is financially supported by the National Key R&D Program of China (Grant 2022YFC3004302) and the Natural Science Foundation of China (Grants No.41929001, 41874005)
More Information
Received Date:  20 August 2022
Revised Date:  14 October 2022
Publish Date:  28 December 2022
    Abstract

  • The lower stream of the Yarlung Zangbo River is in the front zone of the collision between the Indian and Eurasian plates with active neotectonics movements and many high mountains in this region. It is a typical mountain-valley area. Due to the unique geological structure and the influence of climate change, geohazards such as collapses, landslides, and mudslides frequently happen in this area. We used Sentinel-1 and ALOS/PALSAR-2 images to identify the high-elevation geohazards in the region from 2014 to 2020 by combining multiple time-series InSAR techniques and SAR offset-tracking techniques. The identification results show that there are 260 geohazard-induced deformed areas in the study area, and most of them are located in gullies and peaks at higher elevations. The rock avalanche deformations in the Zebalongba glacier gully have formed several large tension cracks, and once the avalanche falls, they are most likely to form a dam. The back edge of the Dabo landslide, which was reactivated by the Milin earthquake, has completely been detached, and the cracks fully penetrate the left and right sides. Once the landslide destabilizes, it will completely block the Yarlung Zangbo River. This study provides a general method for identifying high-elevation geohazards in high mountain-valley areas and a reference for similar geohazards identification.

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