Collaborative Research: Earthquake swarms and aseismic slip in the Salton Trough: High-resolution imaging of the upper frictional stability transition.

合作研究：索尔顿海槽中的地震群和抗震滑移：上部摩擦稳定性转变的高分辨率成像。

• 批准号: 0943906
• 负责人: Rowena Lohman
• 金额: $ 11.43万
• 依托单位: Cornell University
• 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 2013-05-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0943906&HistoricalAwards=false
• 关键词: Collaborative; Research; Earthquake; swarms; aseismic

Efforts to understand the build-up and release of stress along active fault zones require detailed studies of individual faults and placement of those results in a physical framework consistent with our knowledge about rock mechanics. One particularly intriguing fault zone behavior that has been observed with increasing frequency in recent years involves the interplay between aseismic slip and seismic swarm activity. Slow fault slip has been observed to trigger earthquake swarms in a variety of tectonic environments including subduction zones, volcanic systems, and continental strike-slip faults such as those in close proximity to population centers in Southern California. One region that provides a prime environment to study seismic swarms and aseismic creep is the Imperial Valley/Salton Trough in Southern California. Seismic swarms, large (Mw7) earthquakes, and transient episodes of fault creep are all frequent occurrences along the plate boundary faults within the Salton Trough. The Salton Trough offers a prime opportunity to examine the interplay between these varied types of fault activity, since so many of them are observed within a relatively small geographic area, which also has had very detailed geologic studies and contains one of the world?s densest seismic and geodetic station networks. Detailed studies of aseismic and seismic events offer an opportunity to connect physical properties of the fault-zone such as rock type, depth, and temperature with rock-mechanical properties such as frictional stability, and will allow us to better understand the temporal evolution of seismic hazard associated with individual fault zones.We propose a combination of an active source seismic study of the 2005 swarm's primary fault zone, and a more detailed analysis of the existing seismic and geodetic data. The core of our effort is a one-week seismic survey using the high-res profiling techniques developed by the USGS-Menlo Park group that will provide constraints on the details of fault-zone geometry and rigidity structure. These results will be used to improve our studies of the 2005 swarm. The combination of these studies will allow us to study the relations between rock-type, rigidity, thermal structure and frictional stability. Because shallow creep and earthquake swarms are general properties of major faults in the Salton Trough, our results will provide inputs to physics based earthquake hazard models in the region.

要了解活动断层带上应力的积累和释放，需要对各个断层进行详细研究，并将这些结果放置在与我们的岩石力学知识相一致的物理框架中。 近年来，人们越来越频繁地观察到一种特别有趣的断层带行为，即地震滑动和地震群活动之间的相互作用。据观察，缓慢的断层滑动会在各种构造环境中引发地震群，包括俯冲带、火山系统和大陆走滑断层，例如靠近南加州人口中心的断层。 南加州的帝王谷/索尔顿海槽是为研究地震群和地震蠕变提供最佳环境的地区之一。 地震群、大地震（Mw7）和断层蠕动的瞬时事件都是沿着索尔顿海槽内的板块边界断层经常发生的。 索尔顿海槽为研究这些不同类型的断层活动之间的相互作用提供了绝佳的机会，因为其中许多断层活动是在相对较小的地理区域内观察到的，该区域也进行了非常详细的地质研究，并且包含世界上最密集的地震和大地测量站网络之一。对地震和地震事件的详细研究提供了将断层带的物理特性（如岩石类型、深度和温度）与岩石力学特性（如摩擦稳定性）联系起来的机会，并使我们能够更好地了解与各个断层带相关的地震危险性的时间演变。我们建议结合对 2005 年群主断层带的主动源地震研究以及对现有地震和大地测量的更详细分析 数据。 我们工作的核心是使用美国地质勘探局门洛帕克小组开发的高分辨率剖面技术进行为期一周的地震勘测，该技术将为断层带几何形状和刚性结构的细节提供约束。 这些结果将用于改进我们对 2005 年蜂群的研究。这些研究的结合将使我们能够研究岩石类型、刚性、热结构和摩擦稳定性之间的关系。 由于浅层蠕变和地震群是索尔顿海槽主要断层的一般特性，因此我们的结果将为该地区基于物理的地震灾害模型提供输入。