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Collaborative Research: Simultaneous Inversions of GPS Time Series for Kinematics and Transients in Cascadia

Collaborative Research: Simultaneous Inversions of GPS Time Series for Kinematics and Transients in Cascadia
合作研究:卡斯卡迪亚运动学和瞬变的 GPS 时间序列同步反演
批准号:
0946634
负责人:
Robert King
金额:
$9.84万
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2010
资助国家:
美国
项目状态:
已结题
起止时间:
2010-04-01 至 2012-03-31

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中文摘要
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英文摘要
In recent years continuously operating GPS sites have been established in many parts of the world, including Earthscope's Plate Boundary Observatory network in the western US. Prior to that, most GPS observations were made in survey-mode, where campaigns were used to occupy the marks on a yearly or multi-year basis. This project is to explore how to extract long-term plate kinematics and time-dependent deformation information from both continuous and survey-mode GPS data. The science target is to learn about the spatial and temporal relationship between slow slip and non-volcanic tremor throughout Cascadia. The continuous networks of PBO and PANGA are being used to test whether or not slow slip beneath Cascadia coincides spatially and temporally with non-volcanic tremor. Southern Cascadia has a very different pattern of slow-slip than northern Cascadia where slow-slip events are very regular and similar in size. Non-volcanic tremor suggests that there may be some, but different, patterns in southern Cascadia but tremor does not constrain the sizes of the slow slip events. Utilizing the time series directly in the analyses and applying new GPS processing techniques will enhance the signal-to-noise ratio of the vertical component which is critical in estimating the up-dip extent of slow slip on the Cascadia interface. One goal is to test whether or not non-volcanic tremor (NVT) coincides with slow slip. Since NVT is easier to observe than slow slip for small events, their coincidence will help delineate the portions of faults that slip slowly. The work will place important bounds on the up-dip limit of slow slip at Cascadia and hence whether or not slow slip extends into the locked portions of the megathrust. The research will further our understanding of slow-slip events and how they should be presented to the public. The simple question of whether they increase or decrease the earthquake hazard is not yet answered but is of obvious importance.
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  • 批准号:
    24ZR1403900
  • 项目类别:
    省市级项目
  • 资助金额:
    --
  • 批准年份:
    2024
  • 负责人:
    SATOSHI NAWATA
  • 依托单位:
Cell Research
Cell Research
Cell Research (细胞研究)