采用双差定位法对2013年7月22日甘肃岷县-漳县交界地区M6.6地震及主震后48小时内388次余震序列进行重新定位,得到350个精定位地震数据。结果表明,余震优势展布以北东向较大倾角的铲状结构为特征,长约12 km,以主震为中心两侧对称分布;震源深度主要集中在4-10 km范围内,但余震震级由10 km左右深度的3-4级向3 km深度之上近地表的2-3级迁移变化;余震分布清晰呈现双层结构,较深层分布在4-10 km深度,而较浅层分布3 km深度之上,2层之间地震分布较少。分析认为,浅层地震可能为本次地震地表破坏较强原因之一。震源深度剖面显示,破裂面向NE倾斜,推测此次地震的发震断裂为临潭-宕昌断裂。
Applying the double-difference algorithm to the Minxian-Zhangxian, mainshock (M6.6) and its 388 aftershocks after 48 hours, Gansu on July 22 2013, we obtained 350 relocated earthquakes. Our results show that the aftershocks are shown as a shovel-shaped structure with a large northeastward dip extending for over 12 km long along the north-west direction and have an approximately symmetrical distribution about a center of the mainshock. The aftershocks are focused at depths of 4-10 km, but they migrate from about 10 km depth to above 3 km depth and their magnitudes range from 3-4 in a deeper layer to 2-3 in a shallower layer. The aftershocks show clearly a double-layer structure, one of which is at 4-10 km depth, while the other is above 3 km depth. There are few events between these two layers. The shallow earthquake layer could be one of causes that made a strong damage in the event. The vertical cross section of aftershock hypocenters shows a northeast tilt of the fault plane, suggesting that the seismogenic fault of this mainshock could be the Lintan-Diachang fault.
2017,38(2): 12-16 收稿日期:2016-04-27
DOI:10.3969/j.issn.1003-3246.2017.02.003
基金项目:中国地震局地震科技星火计划(项目编号:XH17049Y)
作者简介:梁姗姗(1989-),女,工程师,主要从事小地震定位和震源机制反演工作。E-mail:liangshanshan@seis.ac.cn
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