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CAREER: Investigating the Relationship between Fault Damage Zones and Earthquakes through Seismic Observations and Earthquake Cycle Simulations

职业：通过地震观测和地震周期模拟研究断层破坏区与地震之间的关系

基本信息

批准号：
1943742
负责人：
Yihe Huang
金额：
$ 60万
依托单位：
Regents of the University of Michigan - Ann Arbor
依托单位国家：
美国
项目类别：
Continuing Grant
财政年份：
2020
资助国家：
美国
起止时间：
2020-03-01 至 2025-02-28
项目状态：
未结题

来源：
https://www.nsf.gov/awardsearch/showAward?AWD_ID=1943742&HistoricalAwards=false
关键词：
CAREER Investigating Relationship between Fault

项目摘要

Instead of single planes, faults are volumes of rocks containing centimeters-thick fault cores surrounded by hundreds-meter-thick fractured rocks, called fault damage zones. As discovered worldwide, fault damage zones around major faults accommodate a significant portion of plate motion through seismic and aseismic deformation. However, the poorly understood link between fault damage zones and earthquake source processes remains a fundamental issue that hinders the advancement of earthquake physics research and seismic hazard mitigation. Using a combination of new fault zone imaging methods and fully dynamic earthquake cycle models, the project aims to understand how fault damage zones impact the generation of earthquakes that occur within seconds and how the structure of fault damage zones involves over hundreds of years under the influence of earthquakes and interseismic slip. The project will also promote and enrich the learning experiences of a wide range of students and increase the diversity of students majoring in geophysics. The research lies on the interface of seismic data analysis, earthquake modeling, and fault zone geology, providing a unique opportunity to synergize various research facets and promote communication between different research communities.The current understanding of earthquake source physics is limited by the lack of constraints on the spatial distribution of fault damage zones and their effects on seismicity and interseismic deformation. Previous fault zone studies have relied on near-fault seismic arrays to obtain a cross-sectional view at the array location. The project will image the along-strike variation of fault damage zones and characterize site effects using broadband seismic networks to investigate whether fault damage zones strongly affect seismicity patterns. The project will also improve the understanding of stress drop variation by considering the effects of fault zone waves on earthquake source spectra. Moreover, previous simulations of earthquakes in fault zones have modeled either single earthquakes using arbitrary stress conditions or earthquake cycles without dynamic waves. The project will model earthquakes and interseismic deformation by considering damage rheology and dynamic effects of the fault zone wavefield. The seismic observations and earthquake cycle simulations together will unveil how fault damage zones influence earthquake source processes and how earthquakes and interseismic deformation contribute to the formation of fault damage zones. Additionally, the project will involve graduate students to design and lead hands-on geophysical activities related to the research for Earth Camp, a UM outreach program that provides week-long experiences to educate underrepresented high school students. It will promote the communication between non-science majors and graduate students by introducing poster fairs in a first-year undergraduate seminar course, and strengthen the research skills of students by developing research projects in upper-level undergraduate and graduate courses.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.

断层不是单一平面，而是包含厘米厚断层核的大量岩石，周围环绕着数百米厚的裂缝岩石，称为断层损害区。正如世界范围内发现的那样，主要断层周围的断层破坏带通过地震和地震变形容纳了大部分的板块运动。然而，对断层破坏带和震源过程之间的联系知之甚少，这仍然是一个根本性的问题，阻碍了地震物理学研究和减轻地震灾害的进展。利用新的断层带成像方法和完全动态的地震周期模型相结合，该项目旨在了解断层破坏区如何影响几秒钟内发生的地震的生成，以及断层破坏区的结构如何在地震和地震间滑动的影响下涉及数百年。该项目还将促进和丰富各类学生的学习经验，并增加主修物理学的学生的多样性。该研究位于地震数据分析、地震模拟和断层带地质学的接口上，为协同各个研究方面和促进不同研究社区之间的交流提供了独特的机会。目前对震源物理学的理解受到断层破坏区空间分布及其对地震活动性和地震间变形影响的限制。以前的断层带研究依赖于近断层地震阵列来获得阵列位置的横截面视图。该项目将利用宽带地震网络对断层破坏带沿走向的变化进行成像，并描述场地效应，以调查断层破坏带是否强烈影响地震活动模式。该项目还将通过考虑断层带波对地震源谱的影响来提高对应力降变化的理解。此外，以前对断层带地震的模拟要么使用任意应力条件模拟单次地震，要么模拟没有动态波的地震周期。该项目将通过考虑断裂带波场的损伤流变学和动态效应来模拟地震和震间变形。地震观测和地震周期模拟将揭示断层破坏带如何影响震源过程，以及地震和震间变形如何促成断层破坏带的形成。此外，该项目将涉及研究生设计和领导与地球营研究相关的实践地球物理活动，这是一个UM外联计划，提供为期一周的经验，以教育代表性不足的高中生。通过在大学一年级的研讨课程中引入海报展览会，促进非理科专业学生与研究生之间的交流，并通过在高年级的本科和研究生课程中开发研究项目，加强学生的研究技能。该奖项反映了NSF的法定使命，通过使用基金会的智力价值和更广泛的影响审查标准进行评估，被认为值得支持。