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Seismicity as a Function of Cumulative Geologic Offset: Test of a Hypothesis

Seismicity as a Function of Cumulative Geologic Offset: Test of a Hypothesis
地震活动作为累积地质偏移量的函数：假设检验
批准号：
9005092
负责人：
Steven Wesnousky
金额：
$12.0万
依托单位：
Board of Regents, NSHE, obo University of Nevada, Reno
依托单位国家：
美国
项目类别：
Continuing Grant
财政年份：
1990
资助国家：
美国
项目状态：
已结题
起止时间：
1990-09-01 至 1994-02-28
来源：
https://www.nsf.gov/awardsearch/showAward?AWD_ID=9005092&HistoricalAwards=false
关键词：
SeismicityFunctionCumulativeGeologicOffset

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英文摘要
This research deals with the structural evolution of strike- slip fault zones as related to the statistics of earthquakes in those zones and the geometry of the fault traces. Significant results have already been obtained for the San Andreas fault in California and the Anatolian fault in Turkey. The work is to be extended to faults in the Mojave Desert in California and strike- slip faults in Japan. These ideas have not only yielded new physical insights into faulting but have important implications for earthquake hazard assessment. This research is a component of the National Earthquake Hazard Reduction Program.
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Collaborative Research: Paleoseismology of the M7.3 1915 Pleasant Valley Earthquake Ruptures
Mechanics of Earthquake Faulting along the Himalayan Convergent Plate Boundary
Collaborative Research: Neotectonics and Structural Development of the Northern Walker Lane
Surface Rupture Earthquakes and the Mechanics of Earthquake Faulting
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