A 3-D Seismic Investigation of the Aseismic to Seismic Transition along the Eurasian-Phillippine Sea Plate Boundary: U.S.-Japan Cooperative Program

欧亚-菲律宾海板块边界沿线的无震到地震转变的 3-D 地震研究:美日合作计划

基本信息

  • 批准号:
    9802264
  • 负责人:
  • 金额:
    $ 15.7万
  • 依托单位:
  • 依托单位国家:
    美国
  • 项目类别:
    Standard Grant
  • 财政年份:
    1998
  • 资助国家:
    美国
  • 起止时间:
    1998-09-15 至 2004-08-31
  • 项目状态:
    已结题

项目摘要

9802264 Moore this award will support a seismic reflection, refraction and passive seismicity program to study underthrusting of oceanic crust along the Nankai Trough off the east coast of Japan. The primary feature to be examined in this experiment is the subduction thrust fault from its aseismic zone in the Trough (trench) to a depth of at least 15 kilometers beneath the continental margin where the thrust is marked by significant seismic activity. The goal of the study is to examine changes in physical properties along the thrust as it changes from aseismic to seismic expression. Understanding this transition from compaction and aseismic slip to brittle failure is a major unknown in understanding lithospheric consumption and earthquake dynamics. This Nankai seismogenic zone marks the location of major destructive earthquakes along the Japanese margin. The project is a collaborative experiment. United State scientists will be responsible for acquiring and interpreting 3-dimensional seismic reflection data from the thrust fault and accreting margin. Japanese colleagues will be responsible for deploying ocean bottom seismometers for seismic refraction and passive seismicity studies. In addition t the basic scientific interpretation to be derived from the data, the experiment is critical to the development of the MARGINS initiative and will provide necessary site location data for future drilling by the international Ocean Drilling Program. ***
9802264摩尔该奖项将支持地震反射,折射和被动地震活动计划,以研究海洋地壳的俯冲沿着日本东海岸的南海海槽。在这个实验中要检查的主要特征是俯冲逆冲断层,从海槽(海沟)中的俯冲带到大陆边缘以下至少15公里的深度,那里的逆冲断层具有明显的地震活动。这项研究的目的是检查物理性质的变化,沿着逆冲断层,因为它的变化,从地震的表达。理解这种从压实和无滑移到脆性破坏的转变是理解岩石圈消耗和地震动力学的一个主要未知数。这个南海地震带标志着日本边缘沿着主要破坏性地震的位置。该项目是一项合作实验。美国科学家将负责获取和解释逆冲断层和增生边缘的三维地震反射数据。日本同事将负责部署海底地震仪,用于地震折射和被动地震活动研究。除了从数据中得出的基本科学解释外,该实验对MARGINS倡议的发展至关重要,并将为国际大洋钻探计划今后的钻探提供必要的现场位置数据。 ***

项目成果

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J. Casey Moore其他文献

Contributions from the combined 7th International Conference on Gas in Marine Sediments and the NATO Advanced Research Workshop on Seafloor Hydrocarbon Seeps, Geology Institute, Azerbaijan Academy of Sciences, Baku, 7–11 October 2002
  • DOI:
    10.1007/s00367-003-0161-y
  • 发表时间:
    2003-10-30
  • 期刊:
  • 影响因子:
    1.400
  • 作者:
    John M. Woodside;Robert E. Garrison;J. Casey Moore;Keith A. Kvenvolden
  • 通讯作者:
    Keith A. Kvenvolden
Large-scale pseudotachylytes and fluidized cataclasites from an ancient subduction thrust fault
来自古代俯冲逆冲断层的大型假速晶石和流化碎裂岩
  • DOI:
    10.1130/g21856.1
  • 发表时间:
    2005
  • 期刊:
  • 影响因子:
    5.8
  • 作者:
    C. Rowe;J. Casey Moore;F. Meneghini;Alexander W. McKeirnan
  • 通讯作者:
    Alexander W. McKeirnan

J. Casey Moore的其他文献

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{{ truncateString('J. Casey Moore', 18)}}的其他基金

Where Have All the Earthquakes Gone?
地震都去哪儿了?
  • 批准号:
    0549017
  • 财政年份:
    2006
  • 资助金额:
    $ 15.7万
  • 项目类别:
    Standard Grant
What Locks Subduction Thrusts?
是什么锁定了俯冲冲断层?
  • 批准号:
    0203664
  • 财政年份:
    2002
  • 资助金额:
    $ 15.7万
  • 项目类别:
    Standard Grant
3D Coherency of the Barbados Seismic Data Volume: Improved Imaging of Faults and Fluid Conduits
巴巴多斯地震数据体的 3D 一致性:改进断层和流体管道的成像
  • 批准号:
    9618166
  • 财政年份:
    1997
  • 资助金额:
    $ 15.7万
  • 项目类别:
    Standard Grant
Faults and Subsurface Fluid Flow: Fundamentals and Applications to Hydrogeology and Petroleum Geology: Conference Travel Support
断层和地下流体流动:水文地质学和石油地质学的基础和应用:会议旅行支持
  • 批准号:
    9706646
  • 财政年份:
    1997
  • 资助金额:
    $ 15.7万
  • 项目类别:
    Standard Grant
Three-Dimensional Seismic Reflection Investigation of Fluid Flow and Structural Evolution: Northern Barbados Ridge
流体流动和结构演化的三维地震反射研究:北巴巴多斯海岭
  • 批准号:
    9116350
  • 财政年份:
    1992
  • 资助金额:
    $ 15.7万
  • 项目类别:
    Standard Grant
Structural and Hydrological Evolution of the Central Oregon Accretionary Prism
俄勒冈州中部吸积棱柱的结构和水文演化
  • 批准号:
    9116368
  • 财政年份:
    1991
  • 资助金额:
    $ 15.7万
  • 项目类别:
    Standard Grant
Effects of Dynamic Processes on Permeablility
动态过程对渗透率的影响
  • 批准号:
    9019799
  • 财政年份:
    1991
  • 资助金额:
    $ 15.7万
  • 项目类别:
    Standard Grant
Fluid Flow and Dehydration Reactions Inferred from Chloride Anomalies at Three Accretionary Complexes
从三个增生杂岩处的氯化物异常推断出流体流动和脱水反应
  • 批准号:
    9116462
  • 财政年份:
    1991
  • 资助金额:
    $ 15.7万
  • 项目类别:
    Standard Grant
How Do Faults Capture Fluid Flow During Initial Deformation of a "High Permeability" Accretionary Prism?
在“高渗透率”增生棱柱的初始变形过程中,断层如何捕获流体流动?
  • 批准号:
    8917705
  • 财政年份:
    1990
  • 资助金额:
    $ 15.7万
  • 项目类别:
    Continuing Grant
Fluid Evolution Along Deformation Paths of Melanges in A Developing Accretionary Complex, Olympic Peninsula, Washington
华盛顿州奥林匹克半岛发展中的增生杂岩中混杂岩变形路径的​​流体演化
  • 批准号:
    9005376
  • 财政年份:
    1990
  • 资助金额:
    $ 15.7万
  • 项目类别:
    Continuing Grant

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