級強(qiáng)震,此次強(qiáng)震造成了重大人員傷亡及大量房屋倒塌。綜合利用國內(nèi)外雷達(dá)衛(wèi)星影像,成功提取了定日地震地表形變場,結(jié)果顯示此次地震的發(fā)震斷裂為近南北走向的登么錯(cuò)斷裂,同震斷層破裂長度約 45km ,并以正斷層運(yùn)動(dòng)為主,且地表形變集中在斷層西側(cè)上盤區(qū)域,最大形變量達(dá) 2.1m 。結(jié)合InSAR相干系數(shù)、地震前后雷達(dá)影像后向散射系數(shù)以及現(xiàn)場調(diào)查,開展了震區(qū)房屋建筑震損分析。結(jié)果表明倒塌房屋集中在斷裂以西上盤,該特征與地表形變強(qiáng)烈區(qū)吻合;且震區(qū)房屋倒塌比例隨距斷裂距離增加呈衰減趨勢。其中登么錯(cuò)西北的長所鄉(xiāng)及周邊村落為房屋倒塌最為嚴(yán)重區(qū)域,部分村落房屋倒塌比例超過 75% ,而震中所在查吉村及臨近區(qū)房屋倒塌現(xiàn)象相對較弱,與野外調(diào)查震中未見斷層地表破裂的震損現(xiàn)象一致。研究成果為地震災(zāi)害評估和震后重建工作提供了重要科學(xué)依據(jù)。-龍?jiān)雌诳W(wǎng)" />

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2025年1月7日西藏定日Ms6.8級強(qiáng)震地表同震形變特征與房屋建筑震損分析

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Coseismic deformation and seismic damage assessment of buildings from the 6.8 earthquake in Dingri, Xizang, on January 7, 2025

TAN Shasha’,YANG Yinghui',XU Qiang',WANG Yunsheng1,ZHAO Weihua’, LUO Yonghong’,CHEN Qiang2,JI Feng' 1.State Key LaboratoryofGeohazard Prevention and Geoenvironment Protection, Chengdu University of Technology, Chengdu 610059,China; 2.SouthwestJotongUniversityDepartmentofRemoteSnsingandInformationEngineeing,Chengdu6China

Abstract:On January7,2025,an earthquake struck Dingri County, Shigatse City, Xizang Autonomous Region,causing widespread building damageand casualties.This study integrates satelite radar imagery from multiple domesticand international sources to derive the surface deformation field of the Dingri earthquake.The results ndicate thatthe earthquake was triggered by coseismic normal faulting along the seismogenic Dengmo Cuo fault,with a rupture length exceeding 45km .The main surface deformation was concentrated on the western flank of the fault, with a maximum displacement of 2.1m .InSAR coherence,pre- and post-earthquake radar backscater coeficients,and field surveys were comprehensively utilized to assessbuilding damage in the affected region.The analysisreveals that the house collpse rate decreases with increasing distance from the fault.The northwest lake shore region of Dengmo Cuo,including Changshuo township and nearby villages,suffered the most severe damage, with the house collapse rate exceeding 75% in some areas.In contrast, regions near the epicenter, such as Chaji village, experienced relatively minor damage, suggesting smaller coseismic fault displacement in the source region. Field investigations further confirmed the absence of significant surface rupture near the epicenter.

Key words: Dingri earthquake; coseismic InSAR deformation; coseismic fault rupture; seismic damageassessment;earthquake field investigation

據(jù)中國地震臺(tái)網(wǎng)測定,2025年1月7日9時(shí)5分,西藏自治區(qū)日喀則市定日縣發(fā)生 級地震,震源深度 10km ,震中位于北緯 ,東經(jīng) (圖1)。(剩余14052字)

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