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The Upper Transition From Seismic To Aseismic Faulting on Subduction Megathrusts

The Upper Transition From Seismic To Aseismic Faulting on Subduction Megathrusts
俯冲巨型逆冲上从地震到抗震断层的上部过渡
批准号:
0648331
负责人:
Chris Marone
金额:
$39.0万
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2007
资助国家:
美国
项目状态:
已结题
起止时间:
2007-04-01 至 2011-03-31

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中文摘要
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英文摘要
Intellectual Merit: This research investigates the cause of the world's largest earthquakes, which occur along subduction plate boundaries. These "megathrust" earthquakes rupture sections of the plate boundary, but we still do not understand how the limits of these rupture patches are determined. Goals of the work are to identify reasons why some sections of subduction plate boundaries fail catastrophically in large earthquakes whereas other sections fail by aseismic creep. Identifying these processes is essential to understanding the seismic cycle and predicting the behavior of subduction zones on time scales relevant to tsunami generation and seismic hazard. The research tests two hypotheses for the up dip limit of the seismogenic zone using a complementary set of laboratory-based approaches that focus on (1) frictional properties, including the effect of lithification and consolidation state, clay mineralogy, effective stress, and drainage conditions on frictional constitutive properties; and (2) fluid transport properties between lithification and consolidation state, composition, permeability, and rheology. Samples from ocean drilling cores, exhumed faults, and synthetic fault gouge will be analyzed in carefully controlled laboratory experiments on natural and synthetic samples over P-T, fluid, mineralogical, cementation, and compaction conditions that span the stability transition. Experiments include friction measurements, consolidation tests, measurement of elastic properties and permeability to constrain elastic stiffness, and measurements of effective stress. Biaxial and frictional shear experiments will be carried out as will uniaxial deformation and flow through tests. Broader Impacts: This research has the potential for significant societal impact from an improved understanding of fault mechanics and earthquake physics including tsunami generation and seismic hazard assessment. The effort also complements the NSF IODP and MARGINS programs. The project will train two graduate students and four undergraduate students with the students also getting opportunities to present the results of their research at professional meetings.
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会议论文
EarthCube Data Infrastructure: Collaborative Proposal: A unified experimental-natural digital data system for analysis of rock microstructure
Collaborative Research: Laboratory and Theoretical Investigations of the Micro-Mechanical Origins of Rate and State Friction on Tectonic Faults
The Spectrum of Fault Slip Behaviors and the Mechanics of Slow Earthquakes
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海外基金
Baryogenesis, Dark Matter and Nanohertz Gravitational Waves from a Dark Supercooled Phase Transition
  • 批准号:
    24ZR1429700
  • 项目类别:
    省市级项目
  • 资助金额:
    --
  • 批准年份:
    2024
  • 负责人:
    YUICHIRO NAKAI
  • 依托单位:
以果蝇为模式研究纤毛过渡纤维(Transition fibers)的形成和功能