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The kinematic evolution of this fault should be closely related to the regional tectonic deformation. However, it is difficult to obtain information on structural deformation of the Chenghai Fault due to the large amount of precipitation and well-developed vegetation. The Chenghai normal faulting may drive drainage reorganization in this region, which provides a new perspective for reconstructing and evaluating the tectonic history. High-resolution digital elevation models (DEM) obtained by remote sensing greatly facilitate the study of drainage evolution and active tectonics. We use two methods (\u03c7-plot and Gilbert metrics) to measure the drainage divide stability based on the ALOS DEM (12.5 m resolution) and further reproduce the drainage evolution process in response to the asymmetric uplift by numerical modeling. The results show that the Chenghai\u2013Jinsha drainage divide, hosted by the footwall block of the Chenghai Fault, is migrating westward (away from the Chenghai Fault) and will continue moving ~2.2\u20133.5 km to reach a steady state. Its migration is controlled by the Chenghai normal faulting. The Chenghai\u2013Jinsha drainage divide formed close to the Chenghai Fault\u2019s surface trace and continues to migrate westward in response to the asymmetric uplift. It only took a few million years for the Chenghai\u2013Jinsha drainage divide to migrate to its current location based on the numerical modeling. The restoration of the drainage reorganization implies that the Chenghai Fault initiated in the Pliocene, which probably results from kinematic reversal along the Red River Fault.<\/jats:p>","DOI":"10.3390\/rs16183471","type":"journal-article","created":{"date-parts":[[2024,9,19]],"date-time":"2024-09-19T03:34:20Z","timestamp":1726716860000},"page":"3471","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":5,"title":["Westward Migration of the Chenghai\u2013Jinsha Drainage Divide and Its Implication for the Initiation of the Chenghai Fault"],"prefix":"10.3390","volume":"16","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-1902-573X","authenticated-orcid":false,"given":"Shuang","family":"Bian","sequence":"first","affiliation":[{"name":"State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-0656-6980","authenticated-orcid":false,"given":"Xibin","family":"Tan","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Mountain Hazards and Engineering Resilience, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610299, China"}]},{"given":"Yiduo","family":"Liu","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Mountain Hazards and Engineering Resilience, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610299, China"}]},{"given":"Feng","family":"Shi","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China"}]},{"given":"Junfeng","family":"Gong","sequence":"additional","affiliation":[{"name":"Key Laboratory of Geoscience Big Data and Deep Resource of Zhejiang Province, School of Earth Sciences, Zhejiang University, Hangzhou 310027, China"}]}],"member":"1968","published-online":{"date-parts":[[2024,9,19]]},"reference":[{"key":"ref_1","doi-asserted-by":"crossref","first-page":"419","DOI":"10.1126\/science.189.4201.419","article-title":"Cenozoic Tectonics of Asia: Effects of a Continental Collision: Features of recent continental tectonics in Asia can be interpreted as results of the India-Eurasia collision","volume":"189","author":"Molnar","year":"1975","journal-title":"Science"},{"key":"ref_2","doi-asserted-by":"crossref","first-page":"2905","DOI":"10.1029\/JB082i020p02905","article-title":"Active faulting and tectonics in China","volume":"82","author":"Tapponnier","year":"1977","journal-title":"J. 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