Constraining Early-stage Rifting Through Rapid Response to the Lake Malawi Earthquake Sequence of December 2009

通过对 2009 年 12 月马拉维湖地震序列的快速反应来限制早期裂谷

基本信息

  • 批准号:
    1019379
  • 负责人:
  • 金额:
    $ 1.3万
  • 依托单位:
  • 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
  • 起止时间:
    2010-06-01 至 2011-05-31
  • 项目状态:
    已结题

项目摘要

This RAPID proposal addresses nine earthquakes of magnitude 5 and larger that have taken place in the northern Malawi segment of the East African Rift (EAR) system. These events are extremely rare, and their swarm-like characteristics are highly unusual for this particular region and for the Western Branch of the EAR as a whole. They will deploy a network of 10 seismic stations in the region of these earthquakes to record further main shocks (if they occur) and aftershocks and to relocate these events to better constrain the fault(s) or other subsurface features that are causing them. In particular they will evaluate: (1) whether current events indicate that extension is being accommodated on the major basin-bounding border fault, or whether the extensional strain is occurring primarily on secondary faults in the hanging wall of the major system; and (2) whether deep magmatic activity is associated with the events. These earthquakes offer a rare and important opportunity to address key aspects of deformation and seismogenesis in an early stage rift. Accurate aftershock locations require observations from the epicentral region, where there is currently only one operating seismometer. A rapid deployment is necessary.The December 2009 earthquake sequence has resulted in threecasualties, hundreds of injuries and thousands of displaced people. Aftershocksassociated with the sequence continue, and given the swarm-like character of the dozen or so largest events, it is possible that additional damaging events are still to come. Malawi currently has very limited capacity to monitor and locate these earthquakes; they have no permanent national network, and as of this writing only two seismic stations are in northern Malawi region recording these events.The PIs will work closely with the Geological Survey of Malawi (GSM) in earthquake detection and location techniques, as well as with the USGS, USAID, and the US Embassy to coordinate with the other outreach and humanitarian efforts underway.
该 RAPID 提案涉及东非裂谷 (EAR) 系统马拉维北部地区发生的 9 次 5 级及以上地震。这些事件极为罕见,其群体性特征对于这个特定地区以及整个 EAR 西部分支来说是非常不寻常的。他们将在这些地震地区部署一个由 10 个地震台组成的网络,以记录进一步的主震(如果发生)和余震,并重新定位这些事件,以更好地限制引起这些地震的断层或其他地下特征。他们将特别评估:(1)当前事件是否表明主要盆地边界边界断层正在适应伸展,或者伸展应变是否主要发生在主要系统上盘的次要断层上; (2)深部岩浆活动是否与该事件有关。这些地震为解决早期裂谷变形和地震发生的关键问题提供了难得而重要的机会。准确的余震位置需要从震中地区进行观测,目前该地区只有一台正在运行的地震仪。快速部署是必要的。2009 年 12 月的地震序列已造成三人伤亡、数百人受伤以及数千人流离失所。与该序列相关的余震仍在继续,并且考虑到十几起最大事件的群状特征,可能还会发生更多破坏性事件。马拉维目前监测和定位这些地震的能力非常有限;他们没有永久的国家网络,截至撰写本文时,马拉维北部地区只有两个地震台记录这些事件。PI 将与马拉维地质调查局 (GSM) 在地震探测和定位技术方面密切合作,并与马拉维地质调查局 (GSM) 密切合作。美国地质调查局、美国国际开发署和美国大使馆协调正在进行的其他外展和人道主义工作。

项目成果

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James Gaherty其他文献

James Gaherty的其他文献

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{{ truncateString('James Gaherty', 18)}}的其他基金

Collaborative Research: Quantifying melt in the mantle and controls on lithosphere-asthenosphere dynamics and intraplate magmatism: a joint seismic and EM survey of the Cocos plate
合作研究:量化地幔熔化并控制岩石圈-软流圈动力学和板内岩浆作用:科科斯板块的联合地震和电磁调查
  • 批准号:
    2146911
  • 财政年份:
    2022
  • 资助金额:
    $ 1.3万
  • 项目类别:
    Continuing Grant
Asthenospheric melting and melt-induced evolution of the lithosphere beneath the Colorado Plateau and the Basin and Range from a seismic characterization of mantle layering
根据地幔分层的地震特征研究科罗拉多高原和盆地山脉下方岩石圈的软流圈熔融和熔融引起的演化
  • 批准号:
    2045264
  • 财政年份:
    2020
  • 资助金额:
    $ 1.3万
  • 项目类别:
    Standard Grant
Collaborative Research: Imaging small-scale convection and structure of the mantle in the south Pacific: a US contribution to international collaboration PacificArray
合作研究:对南太平洋小规模对流和地幔结构进行成像:美国对国际合作的贡献 PacificArray
  • 批准号:
    2051265
  • 财政年份:
    2020
  • 资助金额:
    $ 1.3万
  • 项目类别:
    Continuing Grant
Asthenospheric melting and melt-induced evolution of the lithosphere beneath the Colorado Plateau and the Basin and Range from a seismic characterization of mantle layering
根据地幔分层的地震特征研究科罗拉多高原和盆地山脉下方岩石圈的软流圈熔融和熔融引起的演化
  • 批准号:
    1853296
  • 财政年份:
    2019
  • 资助金额:
    $ 1.3万
  • 项目类别:
    Standard Grant
Collaborative Research: Imaging small-scale convection and structure of the mantle in the south Pacific: a US contribution to international collaboration PacificArray
合作研究:对南太平洋小规模对流和地幔结构进行成像:美国对国际合作的贡献 PacificArray
  • 批准号:
    1658491
  • 财政年份:
    2017
  • 资助金额:
    $ 1.3万
  • 项目类别:
    Continuing Grant
Love-wave propagation in oceanic upper mantle: constraints on radial anisotropy and implications for dynamics of the asthenosphere
海洋上地幔中的拉夫波传播:径向各向异性的约束及其对软流圈动力学的影响
  • 批准号:
    1538229
  • 财政年份:
    2015
  • 资助金额:
    $ 1.3万
  • 项目类别:
    Standard Grant
Collaborative Research: Investigating Temperature, Melting, and Mantle Flow in the North American Upper Mantle with 3-D Models of Shear Velocity, Radial Anisotropy, and Attenuation
合作研究:利用剪切速度、径向各向异性和衰减的 3D 模型研究北美上地幔的温度、熔化和地幔流动
  • 批准号:
    1252039
  • 财政年份:
    2013
  • 资助金额:
    $ 1.3万
  • 项目类别:
    Continuing Grant
Thermal structure, hydration and dehydration of the entire Juan de Fuca Plate
整个胡安德富卡板块的热结构、水化和脱水
  • 批准号:
    1334831
  • 财政年份:
    2013
  • 资助金额:
    $ 1.3万
  • 项目类别:
    Standard Grant
Collaborative Research: Faulting processes during early-stage rifting: analysis of an unusual earthquake sequence in northern Malawi
合作研究:早期裂谷期间的断层过程:马拉维北部异常地震序列的分析
  • 批准号:
    1049620
  • 财政年份:
    2010
  • 资助金额:
    $ 1.3万
  • 项目类别:
    Standard Grant
Collaborative Research: Structure and Composition of Oceanic Lithosphere and the Lithosphere/Asthenosphere Boundary
合作研究:海洋岩石圈的结构和组成以及岩石圈/软流圈边界
  • 批准号:
    0928270
  • 财政年份:
    2010
  • 资助金额:
    $ 1.3万
  • 项目类别:
    Continuing Grant

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