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Temporal Seismic Observation and Preliminary Hypocenter Determination of Aftershocks of the 2003 Bam Earthquake, Southeastern Iran

机译:伊朗东南部2003年班姆地震余震的时间地震观测和初步震源测定

摘要

We investigate the hypocenter distribution of aftershocks of the 26 December, 2002 Bam earthquake Mw 0.5 using a temporal seismic network installed for 1 month from 6 February, 2004. Preliminary hypocenters were determined using automatic phase-picking and calculating software. The epicenters are distributed linearly about 20km in length parallel 3.5km west of the Bam fault, and extend from the south of Bam city to the heavily damaged area of eastern Bam city including Arg-e-Bam. The hypocenters are distributed vertically or slightly leaning toward the east in the depth range from 0km to 15 km. Using the hypocenter distribution we propose a schematic 3-D structure model of the source fault distinguished from the Bam fault. Eastern Bam city is located just above the northern part of the source fault and also on the rupture propagation direction from the asperity. It may be a major reason why eastern Bam city suffered the heaviest damage.
机译:我们使用从2004年2月6日起安装了1个月的临时地震网络调查了2002年12月26日Bam地震Mw 0.5的余震的震中分布。初步震源是使用自动相位提取和计算软件确定的。震中在巴姆断层以西3.5公里处线性分布,长度约20公里,从巴姆市南部延伸到东部巴姆市受严重破坏的地区,包括Arg-e-Bam。震源在0 km至15 km的深度范围内垂直分布或略微向东倾斜。利用震源分布,我们提出了与Bam断层不同的源断层的示意性3-D结构模型。东巴姆市位于震源断层北部的正上方,并且从凹凸不平处位于破裂传播方向。这可能是东部班姆市遭受最重破坏的主要原因。

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