{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,5,7]],"date-time":"2026-05-07T17:50:27Z","timestamp":1778176227493,"version":"3.51.4"},"reference-count":52,"publisher":"MDPI AG","issue":"16","license":[{"start":{"date-parts":[[2022,8,18]],"date-time":"2022-08-18T00:00:00Z","timestamp":1660780800000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"name":"China Three Gorges Corporation YMJ(XLD)\/(19)110, China Geology Survey Project","award":["DD20221738-2"],"award-info":[{"award-number":["DD20221738-2"]}]},{"name":"China Three Gorges Corporation YMJ(XLD)\/(19)110, China Geology Survey Project","award":["2018YFC1505002"],"award-info":[{"award-number":["2018YFC1505002"]}]},{"name":"China Three Gorges Corporation YMJ(XLD)\/(19)110, China Geology Survey Project","award":["41672359"],"award-info":[{"award-number":["41672359"]}]},{"name":"National Key R&amp;D Program of China","award":["DD20221738-2"],"award-info":[{"award-number":["DD20221738-2"]}]},{"name":"National Key R&amp;D Program of China","award":["2018YFC1505002"],"award-info":[{"award-number":["2018YFC1505002"]}]},{"name":"National Key R&amp;D Program of China","award":["41672359"],"award-info":[{"award-number":["41672359"]}]},{"DOI":"10.13039\/501100008982","name":"National Science Foundation of China","doi-asserted-by":"publisher","award":["DD20221738-2"],"award-info":[{"award-number":["DD20221738-2"]}],"id":[{"id":"10.13039\/501100008982","id-type":"DOI","asserted-by":"publisher"}]},{"DOI":"10.13039\/501100008982","name":"National Science Foundation of China","doi-asserted-by":"publisher","award":["2018YFC1505002"],"award-info":[{"award-number":["2018YFC1505002"]}],"id":[{"id":"10.13039\/501100008982","id-type":"DOI","asserted-by":"publisher"}]},{"DOI":"10.13039\/501100008982","name":"National Science Foundation of China","doi-asserted-by":"publisher","award":["41672359"],"award-info":[{"award-number":["41672359"]}],"id":[{"id":"10.13039\/501100008982","id-type":"DOI","asserted-by":"publisher"}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Remote Sensing"],"abstract":"<jats:p>In recent years, due to adverse geological conditions, intense human engineering activities, and extreme weather conditions, catastrophic landslides have frequently occurred in southwest China, causing severe loss of life and property. Identifying the kinematic features of potential landslides can effectively support landslide hazard prevention. This study proposes a remote sensing identification method for rotational, planar traction, and planar thrust slides based on geomorphic features as well as vertical and slope-oriented deformation rates. Rotational landslides are characterized by similar vertical and horizontal deformation rates, with vertical deformation mainly occurring at the head and gradually decreasing along the slope, while horizontal deformation mainly occurs at the foot and gradually increases along the slope. As for the planar slide, the dominant deformation is in the horizontal direction. It is further classified into the planar traction and planar thrust types according to the driving position. The vertical deformation of planar traction slides is concentrated at the foot, while the vertical deformation of planar thrust slides is concentrated at the head of the landslide. We identified 1 rotational landslide, 10 planar traction landslides and 10 planar thrust landslides in the basalt weathering crust area of Guizhou. Field investigations of three landslides verified the method\u2019s accuracy. Combining two-dimensional rainfall and time-series deformations, we found that there is a significant positive correlation between landslide deformation acceleration and precipitation. The landslide kinematic identification method proposed in this paper overcomes the shortcomings of the inability to accurately characterize landslide motion by line-of-sight displacement and realizes the non-contact identification of active landslide motion patterns, which is an essential reference value for geological disaster prevention and control in the study area.<\/jats:p>","DOI":"10.3390\/rs14164014","type":"journal-article","created":{"date-parts":[[2022,8,18]],"date-time":"2022-08-18T23:28:41Z","timestamp":1660865321000},"page":"4014","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":8,"title":["Integration of Vertical and Horizontal Deformation Derived by SAR Observation for Identifying Landslide Motion Patterns in a Basaltic Weathered Crust Region of Guizhou, China"],"prefix":"10.3390","volume":"14","author":[{"ORCID":"https:\/\/orcid.org\/0000-0003-4872-5388","authenticated-orcid":false,"given":"Yifei","family":"Zhu","sequence":"first","affiliation":[{"name":"Key Laboratory of Active Tectonics and Geological Safety, Ministry of Natural Resources, Beijing 100081, China"},{"name":"Research Center of Neotectonism and Crustal Stability, China Geological Survey, Beijing 100081, China"},{"name":"Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China"},{"name":"School of Engineering and Technology, China University of Geosciences (Beijing), Beijing 100083, China"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Xin","family":"Yao","sequence":"additional","affiliation":[{"name":"Key Laboratory of Active Tectonics and Geological Safety, Ministry of Natural Resources, Beijing 100081, China"},{"name":"Research Center of Neotectonism and Crustal Stability, China Geological Survey, Beijing 100081, China"},{"name":"Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Chuangchuang","family":"Yao","sequence":"additional","affiliation":[{"name":"Key Laboratory of Active Tectonics and Geological Safety, Ministry of Natural Resources, Beijing 100081, China"},{"name":"Research Center of Neotectonism and Crustal Stability, China Geological Survey, Beijing 100081, China"},{"name":"Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Zhenkai","family":"Zhou","sequence":"additional","affiliation":[{"name":"Key Laboratory of Active Tectonics and Geological Safety, Ministry of Natural Resources, Beijing 100081, China"},{"name":"Research Center of Neotectonism and Crustal Stability, China Geological Survey, Beijing 100081, China"},{"name":"Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China"},{"name":"School of Engineering and Technology, China University of Geosciences (Beijing), Beijing 100083, China"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Zhenkui","family":"Gu","sequence":"additional","affiliation":[{"name":"Key Laboratory of Active Tectonics and Geological Safety, Ministry of Natural Resources, Beijing 100081, China"},{"name":"Research Center of Neotectonism and Crustal Stability, China Geological Survey, Beijing 100081, China"},{"name":"Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Leihua","family":"Yao","sequence":"additional","affiliation":[{"name":"School of Engineering and Technology, China University of Geosciences (Beijing), Beijing 100083, China"}],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"1968","published-online":{"date-parts":[[2022,8,18]]},"reference":[{"key":"ref_1","doi-asserted-by":"crossref","first-page":"883","DOI":"10.1016\/j.jseaes.2010.04.010","article-title":"Spatial distribution of landslides triggered by the 2008 Ms 8.0 Wenchuan earthquake, China","volume":"40","author":"Dai","year":"2011","journal-title":"J. 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