Investigations of the Updip Limit of the Cascadia Seismogenic Zone

卡斯卡迪亚地震带上倾极限的调查

基本信息

  • 批准号:
    0960879
  • 负责人:
  • 金额:
    $ 75万
  • 依托单位:
  • 依托单位国家:
    美国
  • 项目类别:
    Continuing Grant
  • 财政年份:
    2010
  • 资助国家:
    美国
  • 起止时间:
    2010-04-01 至 2016-03-31
  • 项目状态:
    已结题

项目摘要

Great subduction zone earthquakes, such as the Alaska earthquake in 1964) and tsunamis originate in seismogenic (earthquake generating) zones of subduction zones, where vast tracts of seafloor slide beneath adjacent continental margins. One such region is the Cascadia Subduction Zone, which extends from northernmost California to southern British Columbia, Canada. Great earthquakes occur along this margin at interval of several hundred years; the last was in 1700. Given the population density of the region today, the next is likely to cause considerable damage and loss of life. Learning a much as possible about seismogenic processes in Cascadia is clearly imperative. Much has been learned in recent years about how energy is stored and released in seismogenic zones. Among the most interesting phenomona are episodic tremor and slip (ETS) and very low frequency events (VLFE). These are not earthquakes; instead, the Earth groans, but these processes are not well understood. This deployment of ocean bottom seismometers is part of an international collaboration aimed at investigating these seismic processes. Aside from its obvious societal relevance, the broader impacts of this effort include the international collaboration and its contribution to upcoming broader Cascadia initiative.
俯冲带大地震(如1964年的阿拉斯加地震)和海啸起源于俯冲带的孕震(地震生成)区,在那里,大片的海底滑到相邻大陆边缘之下。卡斯卡迪亚俯冲带就是这样一个地区,它从最北端的加州延伸到加拿大的不列颠哥伦比亚省南部。大地震沿着这片边缘每隔几百年发生一次,最近一次发生在1700年。考虑到该地区目前的人口密度,下一次地震可能会造成相当大的破坏和生命损失。尽可能多地了解卡斯卡迪亚的地震孕育过程显然是必要的。近年来,人们对能量在孕震区是如何储存和释放的有了很多了解。其中最有趣的现象是幕式震颤和滑动(ETS)和甚低频事件(VLFE)。这些不是地震;相反,地球呻吟,但这些过程还没有得到很好的理解。海底地震仪的部署是旨在调查这些地震过程的国际合作的一部分。除了其明显的社会意义外,这一努力的更广泛影响包括国际合作及其对即将推出的更广泛的卡斯卡迪亚倡议的贡献。

项目成果

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Jeffrey McGuire其他文献

Jeffrey McGuire的其他文献

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{{ truncateString('Jeffrey McGuire', 18)}}的其他基金

Collaborative Research: Capturing 4D Variations in Stress, Slip, and Fault-Zone Material Properties: The 2019-2021 Gofar Transform Fault Earthquake Prediction Experiment
合作研究:捕捉应力、滑移和断层带材料特性的 4D 变化:2019-2021 年 Gofar 变换断层地震预测实验
  • 批准号:
    1833279
  • 财政年份:
    2018
  • 资助金额:
    $ 75万
  • 项目类别:
    Continuing Grant
Installation of a Seafloor Geodesy Observatory in the Northern Chille Subduction Zone
在北奇利俯冲带安装海底大地测量观测站
  • 批准号:
    1459095
  • 财政年份:
    2015
  • 资助金额:
    $ 75万
  • 项目类别:
    Continuing Grant
Collaborative Research: Installation of a Real-Time Seafloor Geodetic and Thermal Observatory on the Cascadia Subduction Zone
合作研究:在卡斯卡迪亚俯冲带安装实时海底大地测量和热观测站
  • 批准号:
    1259243
  • 财政年份:
    2013
  • 资助金额:
    $ 75万
  • 项目类别:
    Standard Grant
Frictional Behavior of Oceanic Transform Faults and Influence on Earthquake Characteristics
大洋转换断层的摩擦行为及其对地震特征的影响
  • 批准号:
    1061203
  • 财政年份:
    2011
  • 资助金额:
    $ 75万
  • 项目类别:
    Standard Grant
Episodic Slow Slip Events and Tremors in Subduction Zones and Relation to Megathrust Earthquakes
俯冲带的偶发性慢滑事件和地震及其与巨型逆冲地震的关系
  • 批准号:
    1015221
  • 财政年份:
    2010
  • 资助金额:
    $ 75万
  • 项目类别:
    Continuing Grant
Collaborative Research: Understanding the Connections Between Strain Transients and Earthquake Swarms
合作研究:了解应变瞬变与地震群之间的联系
  • 批准号:
    0952174
  • 财政年份:
    2010
  • 资助金额:
    $ 75万
  • 项目类别:
    Standard Grant
Collaborative Research: Earthquake swarms and aseismic slip in the Salton Trough: High-resolution imaging of the upper frictional stability transition.
合作研究:索尔顿海槽中的地震群和抗震滑移:上部摩擦稳定性转变的高分辨率成像。
  • 批准号:
    0943480
  • 财政年份:
    2010
  • 资助金额:
    $ 75万
  • 项目类别:
    Standard Grant
Detecting Aseismic Stressing Transients using Stochastic Seismicity Models
使用随机地震活动模型检测抗震应力瞬变
  • 批准号:
    0738641
  • 财政年份:
    2008
  • 资助金额:
    $ 75万
  • 项目类别:
    Continuing Grant
Examining Changes in Earthquake Triggering Behavior Across the Ocean-Continent Transition, Gulf of California
检查加利福尼亚湾海洋-大陆过渡区地震触发行为的变化
  • 批准号:
    0548785
  • 财政年份:
    2006
  • 资助金额:
    $ 75万
  • 项目类别:
    Standard Grant
A Seafloor Geodesy Experiment at the Discovery Transform Fault
发现转换断层的海底大地测量实验
  • 批准号:
    0351143
  • 财政年份:
    2004
  • 资助金额:
    $ 75万
  • 项目类别:
    Standard Grant

相似海外基金

Determining the Locking State of the Updip end of the Cascadia Megathrust using Real Time Seafloor Geodetic data
使用实时海底大地测量数据确定卡斯卡迪亚巨型逆冲断层上倾端的锁定状态
  • 批准号:
    1825861
  • 财政年份:
    2018
  • 资助金额:
    $ 75万
  • 项目类别:
    Standard Grant
Toward elucidation of behavior in updip limit of seismogenic zone
阐明地震带上倾极限的行为
  • 批准号:
    17H02952
  • 财政年份:
    2017
  • 资助金额:
    $ 75万
  • 项目类别:
    Grant-in-Aid for Scientific Research (B)
Collaborative Research: Post-seismic response updip of the Chilean megathrust earthquake of February 27, 2010
合作研究:2010 年 2 月 27 日智利巨型逆冲地震的震后响应上升
  • 批准号:
    1130013
  • 财政年份:
    2011
  • 资助金额:
    $ 75万
  • 项目类别:
    Standard Grant
MARGINS/GeoPRISMS Post-Doctoral Fellowship Research: Evolution of Sediment Physical Properties in the Nankai Subduction Zone and Implications for the Updip Limit of Seismogenesis
MARGINS/GeoPRISMS 博士后研究:南开俯冲带沉积物物理性质的演化及其对地震发生上倾极限的影响
  • 批准号:
    1049591
  • 财政年份:
    2011
  • 资助金额:
    $ 75万
  • 项目类别:
    Standard Grant
Collaborative Research: Post-seismic response updip of the Chilean megathrust earthquake of February 27, 2010
合作研究:2010 年 2 月 27 日智利巨型逆冲地震的震后响应上升
  • 批准号:
    1129574
  • 财政年份:
    2011
  • 资助金额:
    $ 75万
  • 项目类别:
    Standard Grant
Laboratory Frictional Studies of Fault Gouge: A Test of Hypotheses for Controls on the Updip Limit of the Seismogenic Zone Along Subduction Thrusts
断层泥的室内摩擦研究:控制沿俯冲冲断层发震带上倾极限的假设检验
  • 批准号:
    0196462
  • 财政年份:
    2001
  • 资助金额:
    $ 75万
  • 项目类别:
    Standard Grant
Laboratory Frictional Studies of Fault Gouge: A Test of Hypotheses for Controls on the Updip Limit of the Seismogenic Zone Along Subduction Thrusts
断层泥的室内摩擦研究:控制沿俯冲冲断层发震带上倾极限的假设检验
  • 批准号:
    0001871
  • 财政年份:
    2000
  • 资助金额:
    $ 75万
  • 项目类别:
    Standard Grant
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