2010年青海玉树Ms7.1级地震地表破裂带和形变特征分析  

The surface rupture and coseismic deformation characteristics of the M_s7.1 earthquake at Qinghai Yushu in 2010

作　　者：张桂芳[1] 屈春燕[1] 单新建[1] 刘云华[1] 宋小刚[1] 

机构地区：[1]中国地震局地质研究所 地震动力学国家重点实验室,北京 100029

出　　处：《地球物理学报》2011年第1期121-127,共7页Chinese Journal of Geophysics

基　　金：国家自然科学基金(40874006);中国地震局地质研究所基本科研业务费(DF-IGCEA-0607-1-19);国家科技支撑计划(2008BAC35B04);地震行业专项(200708013)联合资助

摘　　要：通过对SPOT卫星影像上地表破裂的目视解译,以及对ALOS PALSAR卫星数据进行D-InSAR形变提取和分析,结合地震活动性、震源机制、活动构造等资料,确定了发震断层空间分布、断层性质和同震形变场分布特征.结果显示,玉树地震发生在甘孜玉树断裂带上,总体走向约为300°,断层近乎直立.根据相干性强弱将Ⅰ区地表破裂划分为三段:北段长22 km,中段长5 km,南段长6 km,破裂带总长度约33 km.Ⅱ区内非相干带长约10 km.同震形变场分布在78 km×55 km范围内,主震所在的形变Ⅰ区断层两侧视线向相对位错约为0.78 m,转换成水平位错约为1.5 m;余震所在的Ⅱ区形变相对较小.The surface rupture of the Yushu MS7.1 earthquake was identified through visual interpretation of SPOT images and the coseismic deformation was extracted with differential interferometric SAR using the ALOS PALSAR data. Based on the above results, combining with seismic activity, focal mechanism, active tectonics as well, the complexity of the causative ruptures, the faulting characteristics and the distribution of coseismic deformation were finally determined. The results showed that the Yushu earthquake occurred on the nearly vertical Garzê-Yushu fault, which has an average strike of about 300°. According to the property of SAR coherence data, the surface rupture of zoneⅠextends for about 33 km totally and can be divided into three segments, that is, the northern, middle, and southern segment of length 22 km, 5 km, and 6 km, respectively. There is an incoherence strip about 10 km long in zoneⅡ. The relative dislocation on both sides of the fault is about 0.78 m in the line of sight direction in the rupture zoneⅠ, corresponding to about 1.5 m horizontal movement. The value of displacement in the zone Ⅱ is smaller in contrast with the displacement value of zoneⅠ.

关 键 词：玉树地震 差分干涉测量 地表破裂带 同震形变场 

分 类 号：P315[天文地球—地震学]