...
首页> 外文期刊>Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth >The rupture process during the 1999 Duzce, Turkey, earthquake from joint inversion of teleseismic and strong-motion data
【24h】

The rupture process during the 1999 Duzce, Turkey, earthquake from joint inversion of teleseismic and strong-motion data

机译:1999年土耳其杜兹地震中的破裂过程是由远震和强运动数据共同反演而来

获取原文
获取原文并翻译 | 示例
           

摘要

Teleseismic and strong-motion data are inverted to determine the rupture process during the November 1999 Duzce earthquake in NW Turkey. The fault geometry, rise time and rupture velocity are determined from the aftershock distribution and preliminary inversions of the teleseismic data. Joint inversion of the teleseismic and strong-motion data is then carried out for the slip distribution. We obtain the strike 264degrees, dip 64degrees, rake -172degrees, seismic moment 5.0 x 10(19) N m (M-w 7.1), and average stress drop 7 MPa. This earthquake was characterized by bilateral fault rupture and asymmetric slip distribution. Two asperities (areas of large slip) are identified, the eastern one being 1.5 times larger than the western one. The derived slip distribution is consistent with the aftershock distribution, surface rupture and damage. The point of rupture initiation in this Duzce earthquake coincided with the eastern tip of the aftershock distribution of the August 1999 Izmit earthquake. (C) 2004 Elsevier B.V. All rights reserved.
机译:反转地震数据和强运动数据以确定在土耳其西北部1999年11月的杜兹地震中的破裂过程。断层的几何形状,上升时间和破裂速度由余震分布和远震数据的初步反演确定。然后对滑移分布进行地震和强震数据的联合反演。我们获得了264度的走向,64度的倾角,-172度的前倾角,5.0 x 10(19)N m(M-w 7.1)的地震矩,平均应力降7 MPa。这次地震的特点是双边断裂破裂和滑动分布不对称。确定了两个凹凸不平(滑动较大的区域),东部的粗糙程度比西部的粗糙程度高1.5倍。导出的滑移分布与余震分布,表面破裂和损坏一致。这场Duzce地震的破裂起点与1999年8月Izmit地震余震分布的东端重合。 (C)2004 Elsevier B.V.保留所有权利。

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