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作 者:周甜 朱武[1,2,3] 刘晓宇 郝小叶 ZHOU Tian;ZHU Wu;LIU Xiaoyu;HAO Xiaoye(School of Geological Engineering and Geomatics,Chang’an University,Xi’an 710054,China;Key Laboratory of Ecological Geology and Disaster Prevention,MNR,Xi’an 710054,China;State Key Laboratory of Loess Science,Xi’an 710054,China)
机构地区:[1]长安大学地质工程与测绘学院,西安市710054 [2]自然资源部生态地质与灾害防控重点实验室,西安市710054 [3]黄土科学全国重点实验室,西安市710054
出 处:《大地测量与地球动力学》2024年第7期725-731,共7页Journal of Geodesy and Geodynamics
基 金:国家自然科学基金(42074040);陕西省自然科学基金(2023-JC-JQ-24);中央高校基本科研业务费专项(300102262902,300102263401,300102262512,300102263502)。
摘 要:采用覆盖门源地区的C波段Sentinel-1卫星与L波段ALOS-2卫星遥感数据,运用差分干涉(D-InSAR)、像素偏移量追踪(POT)以及多孔径InSAR(MAI)技术,获取2022年青海门源M_(W)6.6地震同震视线向和方位向地表形变场。结合地表应力应变模型与方差分量估计(SM-VCE)方法,推导出地震三维同震位移。采用非线性和线性方法反演断层倾角、走向等几何参数和同震滑动分布特征。结果表明,该地震为左旋走滑型地震,断层自震中向北西-南东方向延伸,最大水平位移达1.58 m,且主要滑动集中在地下0~8 km范围内,最大滑动量为3.54 m,反演的矩震级为M_(W)6.67。We use remote sensing data from the C-band Sentinel-1 and L-band ALOS-2 satellites,which cover the Menyuan area,and apply differential interferometry(D-InSAR),pixel offset tracking(POT),and multi-aperture InSAR(MAI)techniques to obtain the coseismic surface deformation fields of the 2022 Menyuan,Qinghai M_(W)6.6 earthquake in line-of-sight and azimuth directions.By combining the surface stress-strain model with the variance component estimation(SM-VCE)method,we deduce the three-dimensional coseismic displacement.Furthermore,we use both nonlinear and linear approaches to invert the geometric parameters,such as dip angle and strike,as well as the distribution characteristics of coseismic slip.The results reveal that the earthquake was a left-lateral strike-slip event,with the fault extending northwest-southeast from the epicenter.The maximum horizontal displacement reached 1.58 m,and the predominant sliding occurred within a depth range of 0 to 8 km underground,with a maximum slip of 3.54 m.Based on the inversion results,the moment magnitude of earthquake is estimated to be M_(W)6.67.
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