...
首页> 外文期刊>Acta Geophysica Polonica >FOCAL MECHANISM OF EARTHQUAKES FROM THE JUNE 1987 SWARM IN ASWAN, EGYPT, CALCULATED BY THE MOMENT TENSOR INVERSION
【24h】

FOCAL MECHANISM OF EARTHQUAKES FROM THE JUNE 1987 SWARM IN ASWAN, EGYPT, CALCULATED BY THE MOMENT TENSOR INVERSION

机译:1987年6月埃及阿斯旺群震的震源机制,由矩张量反演计算

获取原文
获取原文并翻译 | 示例
           

摘要

We obtained seismic moment tensor solutions of ten events from the June 1987 earthquake swarm, which occurred along the Kalabsha fault zone in the northern part of the Lake Aswan area in Egypt. In addition, the composite fault plane solution of this sequence was also calculated. The waveform data were obtained from the Aswan seismological network, which consists of 13 field stations with short period seismometers GS-13. The June 1987 swarm was a sequence of microearthquakes (M ≤ 3.4), shallow (0-10 km) events forming two successive bursts, which took place on June 17 and 19. The moment tensor solutions indicate that the focal mechanisms of events from this swarm sequence are expressed by right-lateral strike slip faults. They represent also an effective east-west compressional stress field acting in the area. Geological and geophysical data demonstrate that the Kalabsha fault zone is a right-lateral strike slip fault that consists of several fault segments trending in the east-west direction, perpendicular to the axis of the main course of the Lake Aswan. Thus, the focal mechanisms of the 1987 events are consistent with the local tectonics of the area.
机译:我们从1987年6月的地震群中获得了10个事件的地震矩张量解,这些地震群发生在埃及阿斯旺湖地区北部的卡拉布莎断裂带上。另外,还计算了该序列的复合断层平面解。波形数据来自阿斯旺地震网络,该网络由13个带有短周期地震仪GS-13的现场站组成。 1987年6月的群是一系列微地震(M≤3.4),浅(0-10 km)事件,形成了两个连续的爆发,发生在6月17日和19日。瞬间张量解表明,由此引起的事件的焦点机制群序列由右侧走滑断层表达。它们还代表了在该区域起作用的有效的东西向压缩应力场。地质和地球物理数据表明,Kalabsha断层带是一个右旋走滑断层,由沿东西方向延伸的几个断层段组成,垂直于阿斯旺湖主干道的轴线。因此,1987年事件的震源机制与该地区的局部构造一致。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号