{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,10,11]],"date-time":"2025-10-11T01:17:24Z","timestamp":1760145444787,"version":"build-2065373602"},"reference-count":66,"publisher":"MDPI AG","issue":"14","license":[{"start":{"date-parts":[[2024,7,17]],"date-time":"2024-07-17T00:00:00Z","timestamp":1721174400000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"name":"Second Tibetan Plateau Scientific Expedition and Research (STEP)","award":["2019QZKK0901","42072250"],"award-info":[{"award-number":["2019QZKK0901","42072250"]}]},{"name":"National Natural Science Foundation of China","award":["2019QZKK0901","42072250"],"award-info":[{"award-number":["2019QZKK0901","42072250"]}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Remote Sensing"],"abstract":"<jats:p>The Ganzi\u2013Xianshuihe Fault Zone is a large-scale sinistral strike-slip fault zone on the eastern Tibet. As the boundary fault zone of the Bayankala Block and the Chuandian Block, it controls the clockwise rotation of the southeastern Tibet. However, there is still controversy regarding the activity changes between fault zones. Therefore, accurately determining the slip rates of faults in the area is crucial for characterizing regional plate motions and assessing associated seismic hazards. We focused on studying four fault segments near the Ganzi\u2013Xianshuihe Fault Zone, including the Manigango, Ganzi, Luhuo, and Daofu segments. In each segment, we selected typical sinistral piercing points and carried out Unmanned Aerial Vehicle (UAV) photogrammetry to obtain high-resolution terrain data. We utilized LaDiCaoz_V2.2 and GlobalMapper software (LaDiCaoz_V2.2 and Global Mapper v17.0) to measure the offsets, together with optically stimulated luminescence (OSL) dating, to constrain the timing of fault activity. The estimated slip rates for the Manigango, Ganzi, Luhuo, and Daofu segments are as follows: 9.2 \u00b1 0.75 mm\/yr, 9.59 \u00b1 1.7 mm\/yr, 4.23 \u00b1 0.66 mm\/yr, and 7.69 \u00b1 0.76 mm\/yr, respectively. Integrating previous results with slip rates estimated in this study, our analysis suggests the slip rate of the Ganzi\u2013Xianshuihe Fault Zone is around 8\u201310 mm\/year, exhibiting a consistent slip rate from northwest to southeast. This reflects the overall coordination of the movement on the eastern Tibet, with the strike-slip fault zone only controlling the direction of movement.<\/jats:p>","DOI":"10.3390\/rs16142612","type":"journal-article","created":{"date-parts":[[2024,7,17]],"date-time":"2024-07-17T15:15:19Z","timestamp":1721229319000},"page":"2612","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":0,"title":["Spatial Variations of Late Quaternary Slip Rates along the Ganzi\u2013Xianshuihe Fault Zone in the Eastern Tibet"],"prefix":"10.3390","volume":"16","author":[{"ORCID":"https:\/\/orcid.org\/0000-0001-8697-7514","authenticated-orcid":false,"given":"Kai","family":"Sun","sequence":"first","affiliation":[{"name":"State Key Laboratory of Seismic Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-9574-2079","authenticated-orcid":false,"given":"Chuanyou","family":"Li","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Seismic Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-5527-7136","authenticated-orcid":false,"given":"Mingjian","family":"Liang","sequence":"additional","affiliation":[{"name":"Sichuan Earthquake Administration, Chengdu 610041, China"},{"name":"Chengdu Qinghai-Tibet Plateau Earthquake Research Institute, China Earthquake Administration, Chengdu 610041, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-7411-1190","authenticated-orcid":false,"given":"Xinnan","family":"Li","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Seismic Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-7993-2422","authenticated-orcid":false,"given":"Quanxing","family":"Luo","sequence":"additional","affiliation":[{"name":"Surface Process Analysis and Simulation Key Laboratory of Ministry of Education, School of Urban and Environmental Sciences, Peking University, Beijing 100871, China"}]},{"given":"Guangxue","family":"Ren","sequence":"additional","affiliation":[{"name":"China Railway Design Corporation, Tianjin 300251, China"}]},{"ORCID":"https:\/\/orcid.org\/0009-0002-9220-1362","authenticated-orcid":false,"given":"Feipeng","family":"Huang","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Seismic Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China"},{"name":"Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China"}]},{"given":"Junjie","family":"Li","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Seismic Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China"}]}],"member":"1968","published-online":{"date-parts":[[2024,7,17]]},"reference":[{"key":"ref_1","doi-asserted-by":"crossref","first-page":"1671","DOI":"10.1126\/science.105978","article-title":"Oblique stepwise rise and growth of the Tibet plateau","volume":"294","author":"Tapponnier","year":"2001","journal-title":"Science"},{"key":"ref_2","doi-asserted-by":"crossref","first-page":"151","DOI":"10.1016\/0033-5894(88)90020-8","article-title":"Bounds on the Holocene Slip Rate of the Haiyuan Fault, North-Central China","volume":"30","author":"Peizhen","year":"1988","journal-title":"Quat. 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