{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,1,8]],"date-time":"2026-01-08T21:03:49Z","timestamp":1767906229276,"version":"3.49.0"},"reference-count":64,"publisher":"MDPI AG","issue":"4","license":[{"start":{"date-parts":[[2023,2,8]],"date-time":"2023-02-08T00:00:00Z","timestamp":1675814400000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"DOI":"10.13039\/501100001809","name":"National Natural Science Foundation of China","doi-asserted-by":"publisher","award":["41904050"],"award-info":[{"award-number":["41904050"]}],"id":[{"id":"10.13039\/501100001809","id-type":"DOI","asserted-by":"publisher"}]},{"DOI":"10.13039\/501100001809","name":"National Natural Science Foundation of China","doi-asserted-by":"publisher","award":["U2139205"],"award-info":[{"award-number":["U2139205"]}],"id":[{"id":"10.13039\/501100001809","id-type":"DOI","asserted-by":"publisher"}]},{"DOI":"10.13039\/501100001809","name":"National Natural Science Foundation of China","doi-asserted-by":"publisher","award":["CEAIEF2022010100"],"award-info":[{"award-number":["CEAIEF2022010100"]}],"id":[{"id":"10.13039\/501100001809","id-type":"DOI","asserted-by":"publisher"}]},{"name":"Special Fund of the Institute of Earthquake Forecasting","award":["41904050"],"award-info":[{"award-number":["41904050"]}]},{"name":"Special Fund of the Institute of Earthquake Forecasting","award":["U2139205"],"award-info":[{"award-number":["U2139205"]}]},{"name":"Special Fund of the Institute of Earthquake Forecasting","award":["CEAIEF2022010100"],"award-info":[{"award-number":["CEAIEF2022010100"]}]},{"name":"Special Fund of the Institute of Earthquake Forecasting, China Earthquake Administration","award":["41904050"],"award-info":[{"award-number":["41904050"]}]},{"name":"Special Fund of the Institute of Earthquake Forecasting, China Earthquake Administration","award":["U2139205"],"award-info":[{"award-number":["U2139205"]}]},{"name":"Special Fund of the Institute of Earthquake Forecasting, China Earthquake Administration","award":["CEAIEF2022010100"],"award-info":[{"award-number":["CEAIEF2022010100"]}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Remote Sensing"],"abstract":"<jats:p>We used near-field and regional GNSS (Global Navigation Satellite System) data to quantify the deformation and locking ratio of the Xiaojiang fault (XJF) in southeastern Tibet. The inversion based on the dislocation model shows that the slip rate of the XJF is 9\u201311 mm\/a; the locking depths of the northern, central, and southern segments are 25.5 km, 12 km, and 22.5 km, respectively. The inversion with DEFNODE program shows that the locking of the northern segment is the strongest above a depth of 20 km, while the locking between 20 km and 26 km is intermediate, and the weakest locking is found below 26 km. In the central segment, the depths of the interface are 6 km and 12 km. Additionally, a locked asperity that has the potential of generating an Mw 7.2 earthquake along the northern segment is delineated. The asperity and the shallow locking zone are basically consistent with the rupture area of the 1733 M 7.8 Dongchuan earthquake and the 1833 M 8 Songming earthquake, respectively. Both the activity of the historical strong earthquakes and the seismicity of the microearthquakes recorded over recent years seem to suggest that a potential earthquake is imminent.<\/jats:p>","DOI":"10.3390\/rs15040944","type":"journal-article","created":{"date-parts":[[2023,2,9]],"date-time":"2023-02-09T02:55:54Z","timestamp":1675911354000},"page":"944","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":4,"title":["A Potential Earthquake with Magnitude Mw 7.2 on the Northern Xiaojiang Fault Revealed by GNSS Measurement"],"prefix":"10.3390","volume":"15","author":[{"given":"Yun","family":"Zhou","sequence":"first","affiliation":[{"name":"Institute of Geophysics, China Earthquake Administration, Beijing 100081, China"}]},{"given":"Lisheng","family":"Xu","sequence":"additional","affiliation":[{"name":"Institute of Geophysics, China Earthquake Administration, Beijing 100081, China"}]},{"given":"Zhengyang","family":"Pan","sequence":"additional","affiliation":[{"name":"Institute of Earthquake Forecasting, China Earthquake Administration, Beijing 100036, China"}]},{"given":"Ming","family":"Hao","sequence":"additional","affiliation":[{"name":"The Second Monitoring and Application Center, China Earthquake Administration, Xi\u2019an 710054, China"}]},{"given":"Chunlai","family":"Li","sequence":"additional","affiliation":[{"name":"Institute of Geophysics, China Earthquake Administration, Beijing 100081, China"}]}],"member":"1968","published-online":{"date-parts":[[2023,2,8]]},"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","volume":"189","author":"Molnar","year":"1975","journal-title":"Science"},{"key":"ref_2","doi-asserted-by":"crossref","first-page":"1","DOI":"10.1016\/S0012-821X(96)00201-4","article-title":"Age of initiation of collision between India and Asia: A review of stratigraphic data","volume":"145","author":"Rowley","year":"1996","journal-title":"Earth Planet. 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