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EAGER: Bubble Plume Emissions from Fault Zones within the Puget Sound Forearc

EAGER: Bubble Plume Emissions from Fault Zones within the Puget Sound Forearc
EAGER:普吉特湾前弧内断层带的气泡羽流排放
批准号:
1945975
负责人:
Harlan Johnson
金额:
$9.4万
依托单位:
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2019
资助国家:
美国
项目状态:
已结题
起止时间:
2019-09-01 至 2022-08-31

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中文摘要
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英文摘要
This EAGER proposal will obtain samples from newly identified gas and fluid plumes in Puget Sound to determine whether the plumes come from the Cascadia subduction zone megathrust. The idea is that deep regional faults act as pathways for upward migration of fluid that has been generated by heating along the plate interface between the North America and the incoming Juan de Fuca Plate. If the Puget Sound plumes have a subduction zone source, the plumes may provide a means to monitor the pressure and chemistry of the fluid between the plates, and provide a new approach for studying slip on the Cascadia subduction zone megathrust fault. This project is a first step toward developing predictive models for understanding seismic hazards in the heavily-populated Pacific Northwest.Upward migration of fluid and gas through the forearc crust that overlies active subduction zone faults has been observed in settings very similar to the Puget Sound region, including Japan Trench on the Kii peninsula, New Zealand at the Hikurangi margin, and on the Baja California Peninsula, Mexico. Although these fluid seeps emit fluid with helium, oxygen, hydrogen isotope signatures that unambiguously identify them as coming from the subduction zone fault, none of them emit fluid and gas with the vigor or wide spatial distribution observed within Puget Sound. Critically, none of the previous globally-identified forearc plumes are in subduction zones where periodic Episodic Tremor and Slip (ETS) events occur - that arise from periodic local slippage on the subduction zone fault. At Cascadia, these ETS events have a quasi-period of 14 months and variations in the amplitude and intervals are newly-recognized as potential precursors to both regional faulting and large episodic megathrust earthquakes. If the the new Puget plumes are found to be derived from the subduction zone megathrust zone, it would be the first step in using correlations between the variations in emissions and ETS behavior to understand slip on the megathrust.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.
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Methane Venting from Forearc Faults in the Puget Sound Estuary
  • 批准号:
    2221821
  • 项目类别:
    Standard Grant
  • 资助金额:
    $50.86万
  • 财政年份:
    2022
  • 负责人:
    Harlan Johnson
  • 依托单位:
Discriminating slow slip earthquakes and sediment gravity flows from oceanographic signals: the Alaska Amphibious Community Seismic Experiment
  • 批准号:
    1951071
  • 项目类别:
    Standard Grant
  • 资助金额:
    $15.24万
  • 财政年份:
    2020
  • 负责人:
    Harlan Johnson
  • 依托单位:
A proposed study of the dynamics of the Hikurangi New Zealand margin.
  • 批准号:
    1753660
  • 项目类别:
    Standard Grant
  • 资助金额:
    $30.0万
  • 财政年份:
    2018
  • 负责人:
    Harlan Johnson
  • 依托单位:
Remotely Triggered Slope Failures and Turbidity Currents on the Cascadia Margin
  • 批准号:
    1634095
  • 项目类别:
    Standard Grant
  • 资助金额:
    $36.21万
  • 财政年份:
    2016
  • 负责人:
    Harlan Johnson
  • 依托单位:
国内基金
海外基金
红外尘埃Bubble:大质量恒星对其周围分子云环境反馈作用的相关研究
  • 批准号:
    11303081
  • 项目类别:
    青年科学基金项目
  • 资助金额:
    28.0万元
  • 批准年份:
    2013
  • 负责人:
    纪伟光
  • 依托单位: