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2008年3月21日新疆于田7.3级地震发震构造与震前地震活动特征研究
引用本文:李志海,马宏生,曲延军.2008年3月21日新疆于田7.3级地震发震构造与震前地震活动特征研究[J].中国地震,2009,25(2).
作者姓名:李志海  马宏生  曲延军
作者单位:1. 新疆维吾尔自治区地震局,乌鲁木齐市北京南路42号,830011
2. 中国地震局地震预测研究所,北京,100036
基金项目:国家"十一五"科技支撵项且,中国地震局监测预报司课题 
摘    要:2008年3月21日新疆于田发生7.3级地震,打破了中国大陆6年多的7级地震平静,成为我国近期较为显著的一次地震事件.综合分析MS≥4.0余震分布、震区断裂性质以及等震线长轴方向等资料,认为郭扎错断裂是这次地震的发震构造;据Harvard震源机制解分析,这次地震是在近NS向力的作用下,郭扎错断裂发生略带走滑分量的拉张破裂所致.通过地震前震区附近地震活动特征分析发现,于田地震发生在1996年以来新疆南部及邻区7级地震有序分布的空段;震前震区附近有4级地震空区形成,空区持续91个月后发生了2006年9月12日皮山5.8级"信号震",其后1.5年发生于田7.3级地震.

关 键 词:于田地震  发震构造  空区  信号震

Study on Seismogenic Structure and Seismic Activity Characteristics Before the Yutian M7.3 Earthquake on March 21, 2008, Xinjiang
Li Zhihai,Ma Hongsheng,Qu Yanjun.Study on Seismogenic Structure and Seismic Activity Characteristics Before the Yutian M7.3 Earthquake on March 21, 2008, Xinjiang[J].Earthquake Research in China,2009,25(2).
Authors:Li Zhihai  Ma Hongsheng  Qu Yanjun
Abstract:The Yutian Ml .3 earthquake on March 21, 2008, Xinjiang broke the quiescence of more than six years for Ml. 0 earthquake in Chinese Mainland. The analysis of the aftershocks with M_S= 4.0, fault strike direction in seismic region and the long axis of isoseismal shows Gozhaco fault is the seismogenic structure. According to the Harvard focal mechanism, the normal break of Gozhaco fault leads to the Yutian earthquake under the NS direction regional stress. The analysis of the seismic activity before Yutian earthquake shows that the earthquake occurred in the empty area between the belt of M7.0 earthquakes in the southern region of Xinjiang and its adjacent region; there is M_S4.0 seismic gap, and it lasts 91 months. After that, the "signal earthquake" occurred on September 12, 2006 in the seismic gap, 1.5 years prior to the Yutian earthquake.
Keywords:Yutian earthquake Seismogenic structure Seismic gap Signal earthquake
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