{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,10,11]],"date-time":"2025-10-11T01:21:58Z","timestamp":1760145718469,"version":"build-2065373602"},"reference-count":92,"publisher":"MDPI AG","issue":"17","license":[{"start":{"date-parts":[[2024,8,29]],"date-time":"2024-08-29T00:00:00Z","timestamp":1724889600000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"name":"National Nature Science Foundation of China","award":["42202253","ZDJ2019-28","ZDJ2019-21"],"award-info":[{"award-number":["42202253","ZDJ2019-28","ZDJ2019-21"]}]},{"name":"National Institute of Natural Hazards, Ministry of Emergency Management of China","award":["42202253","ZDJ2019-28","ZDJ2019-21"],"award-info":[{"award-number":["42202253","ZDJ2019-28","ZDJ2019-21"]}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Remote Sensing"],"abstract":"<jats:p>The Sichuan-Yunnan block is a tectonically active region in China, with frequent large earthquakes occurring in and around it. Despite most earthquakes being concentrated along boundary faults, intraplate faults also have the potential to generate damaging earthquakes. Remote sensing makes it possible to identify these potential earthquake source faults. During an active fault investigation in the Liangshan area, a distinct lithological boundary named Caimashui fault was found. The geometric distribution and kinematic parameter of the fault is crucial for assessing seismic hazards and understanding the deformation pattern within the Sichuan-Yunnan block. The Caimashui fault is mapped with remote sensing interpretation, a field survey, and UAV measurement. Through trenching and Quaternary dating, the Late Quaternary active characteristics of the fault are studied. The fault is a Holocene active dextral strike-slip fault with a reverse component, exhibiting a dextral strike-slip rate of ~0.70 \u00b1 0.11 mm\/a. Paleoseismic investigation shows that the last surface rupture event of the Caimashui fault occurred later than 4150 \u00b1 30a BP, with a magnitude of M \u2265 7.0. The fault may act as a secondary splitting fault, absorbing the deformation caused by various sinistral strike-slip rates of the boundary faults and the potential energy from the counterclockwise rotation of the Central Yunnan micro-block.<\/jats:p>","DOI":"10.3390\/rs16173203","type":"journal-article","created":{"date-parts":[[2024,8,29]],"date-time":"2024-08-29T11:33:37Z","timestamp":1724931217000},"page":"3203","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":0,"title":["Newly Discovered NE-Striking Dextral Strike-Slip Holocene Active Caimashui Fault in the Central Part of the Sichuan-Yunnan Block and Its Tectonic Significance"],"prefix":"10.3390","volume":"16","author":[{"ORCID":"https:\/\/orcid.org\/0009-0002-0796-7508","authenticated-orcid":false,"given":"Xin","family":"Tan","sequence":"first","affiliation":[{"name":"National Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, China"},{"name":"Sichuan Earthquake Agency, Chengdu 610041, China"}]},{"given":"Kuan","family":"Liang","sequence":"additional","affiliation":[{"name":"National Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, China"},{"name":"Key Laboratory of Compound and Chained Natural Hazards Dynamics, Ministry of Emergency Management of China, Beijing 100085, China"}]},{"given":"Baoqi","family":"Ma","sequence":"additional","affiliation":[{"name":"National Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, China"},{"name":"Key Laboratory of Compound and Chained Natural Hazards Dynamics, Ministry of Emergency Management of China, Beijing 100085, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-5436-5759","authenticated-orcid":false,"given":"Zhongtai","family":"He","sequence":"additional","affiliation":[{"name":"Institute of Geology, China Earthquake Administration, Beijing 100029, China"}]}],"member":"1968","published-online":{"date-parts":[[2024,8,29]]},"reference":[{"key":"ref_1","doi-asserted-by":"crossref","first-page":"611","DOI":"10.1130\/0091-7613(1982)10<611:PETIAN>2.0.CO;2","article-title":"Propagating extrusion tectonics in Asia: New insights from simple experiments with plasticine","volume":"10","author":"Tapponnier","year":"1982","journal-title":"Geology"},{"key":"ref_2","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_3","first-page":"23","article-title":"Neotectonic features of the Ganzi-Yushu fault zone and assessment of its earthquake risk","volume":"7","author":"Wen","year":"1985","journal-title":"Seismol. 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