权益分类	功能权益	普通用户	{{item.name}}会员
{{category.name}}	{{benefitItem.name}}

An Investigation of the Geotechnical Aspects of the November 12, 1999, Duzce, Turkey Earthquake - Preliminary Reconnaissance Effort

对 1999 年 11 月 12 日土耳其迪兹杰地震的岩土工程方面的调查 - 初步勘察工作

基本信息

批准号：
0083058
负责人：
Jonathan Bray
金额：
$ 2.48万
依托单位：
University of California-Berkeley
依托单位国家：
美国
项目类别：
Standard Grant
财政年份：
2000
资助国家：
美国
起止时间：
2000-05-01 至 2002-04-30
项目状态：
已结题

来源：
https://www.nsf.gov/awardsearch/showAward?AWD_ID=0083058&HistoricalAwards=false
关键词：
Investigation Geotechnical Aspects November 12

项目摘要

Abstract0083058A magnitude 7.2 earthquake occurred on November 12, 1999 in the area of Duzce-Bolu, Turkey, 70 km east of Adapazari and 170 km northwest of Ankara, resulting in extensive damage, injuries and loss of life. This earthquake occurred along the North Anatolian fault, a strike slip fault that has many similarities to the San Andreas fault in California.This action provides partial support for a reconnaissance team that was dispatched shortly after the earthquake to document the geotechnical, engineering geology/seismology, and tsunamigenic features of this earthquake in as much detail as possible. This team coordinated with other reconnaissance teams from Turkey, Japan and the United States.As with all post-earthquake reconnaissance investigations, it is expected that vital records and data will become available as a result of this earthquake in Turkey. From a scientific viewpoint, these large earthquakes act as full-scale experiments that cannot be duplicated via controlled experiments in the laboratory or in the field. It is through quick response reconnaissance efforts that the mostly-ephemeral data from these events can be recovered and used to further advances in earthquake hazard mitigation. The results from this investigation are expected to yield information and data that will help the profession to understand the effects of large-scale strike slip fault systems on urbanized and industrial areas.This is a multi-institutional award involving the University of California at Berkeley and the University of Southern California.

1999年11月12日，土耳其杜兹塞-博卢地区（阿达帕扎里以东70公里，安卡拉西北170公里）发生7.2级地震，造成大规模破坏、人员伤亡。这次地震发生在沿着北安纳托利亚断层，这是一个走滑断层，与加州的圣安德烈亚斯断层有许多相似之处。这一行动为地震后不久派出的勘察队提供了部分支持，以尽可能详细地记录这次地震的岩土工程、工程地质/地震学和海啸特征。该小组与来自土耳其、日本和美国的其他侦察小组协调，与所有地震后侦察调查一样，预计土耳其这次地震将提供重要记录和数据。从科学的角度来看，这些大地震是一个全面的实验，无法通过实验室或现场的控制实验来复制。正是通过快速反应的侦察工作，这些事件的大多数短暂的数据可以恢复和用于进一步推进减轻地震灾害。这项研究的结果有望产生信息和数据，这将有助于该专业了解大规模走滑断层系统对城市化和工业区的影响。这是一个涉及加州大学伯克利分校和南加州大学的多机构奖项。