首页> 外文期刊>地震学报(英文版) >A new technique for moment tensor inversion with applications to the 2008 Wenchuan Ms8.0 earthquake sequence
【24h】

A new technique for moment tensor inversion with applications to the 2008 Wenchuan Ms8.0 earthquake sequence

机译:张量反演的新技术及其在2008年汶川Ms8.0地震序列中的应用

获取原文
获取原文并翻译 | 示例
       

摘要

A Ms8.0 earthquake occurred in Wenchuan County, Sichuan Province, China, on May 12, 2008, and subsequently, numerous aftershocks followed. We obtained the moment tensor solutions and source time functions (STFs) for the Wenchuan earthquake and its seven larger aftershocks (Ms5.0~6.0) by a new technique of moment tensor inversion using the broadband and long-period seismic waveform data from the Global Seismic Network (GSN). Firstly, the theoretical background and technical flow of the new technique was briefly introduced, and an aftershock of the Wenchuan earthquake sequence was employed to illustrate the real procedure for inverting the moment tensor; secondly, the moment tensor solutions and STFs of the eight events, including the main shock, were presented, and finally, the interpretation of the results was made. The agreement of our results with the GCMT results indicates the new approach is efficient and feasible. By using this approach, not only the moment tensor solution can be obtained but also the STF can be retrieved; the inverted STFs indicate that the source rupture process may be com-plicated even for the moderate earthquakes. The inverted focal mechanisms of the Wenchuan earthquake sequence show that the most of the aftershocks occurred in the main faults of the Longmenshan fault zone with predomi-nantly thmstingwith minor right-lateral strike-slip component, but some of them may have occurred in the sub-faults with strike-slip faulting in the vicinity of the main faults.
机译:2008年5月12日,中国四川汶川县发生了Ms8.0地震,随后发生了多次余震。利用来自全球的宽带和长周期地震波形数据,通过矩矩张量反演的新技术,获得了汶川地震及其七个较大余震(Ms5.0〜6.0)的矩张量解和震源时间函数(STF)。地震台网(GSN)。首先简要介绍了新技术的理论背景和技术流程,并以汶川地震序列的余震为例,说明了反演张量的真实过程。其次,给出了包括主震在内的8个事件的矩张量解和STF,最后对结果进行了解释。我们的结果与GCMT结果一致,表明新方法是有效且可行的。通过使用这种方法,不仅可以获得矩张量解,而且可以检索STF。反演的STF表示即使对于中等地震,震源破裂过程也可能很复杂。汶川地震序列的倒震震源机制表明,大部分余震发生在龙门山断裂带的主要断层中,主要为隆起,右旋走滑分量较小,但其中一些可能发生在次子中。 -在主要断层附近具有走滑断层的断层。

著录项

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