Intermediate Depth Earthquakes: Investigations of the Predominance and Cause of Subhorizontal Faults

中深度地震：地下断层的优势和成因研究

• 批准号: 1141905
• 负责人: Linda Warren
• 金额: $ 24.74万
• 依托单位: Saint Louis University
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2012
• 资助国家: 美国
• 起止时间: 2012-03-01 至 2016-02-29
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1141905&HistoricalAwards=false
• 关键词: Intermediate; Depth; Earthquakes; Investigations; Predominance

Deep earthquakes were discovered nearly 100 years ago, but how they can occur outside the normal pressure-temperature conditions for brittle failure remains a mystery. Following up on recent observations that earthquakes from ~75-300 km depth often occur along subhorizontal faults, we have developed new hypotheses and tests to investigate the predominance and cause of these faults. Do outer rise faults remain weak as the slab bends and subducts? Alternatively, are the fossil outer rise faults strong because they have healed? Does the stress field in the bending slab result in downward pumping of water that initiates earthquakes? Do sustained fault zones exist? Is rupture propagation an isobaric process? Different seismic observations would support or refute each of these hypotheses, and we have selected two study areas, Japan and Colombia, with features and regional data sets ideal for answering these questions. In Japan, we are using the broadband F-Net records to analyze the directivity of ~500 earthquakes down to magnitude ~4.5. In Colombia, we are collaborating with Professor German Prieto of the Universidad de los Andes to analyze the Cauca cluster of ~2000 earthquakes through relocation and source characterization. These analyses will advance understanding of a long-unresolved question in the Earth sciences. In the process, the participation of a graduate student, an undergraduate student, and an early-career scientist will promote teaching and training, and the international collaboration will enhance the infrastructure for research and education.

深源地震在近100年前就被发现了，但它们如何在正常的压力-温度条件之外发生脆性破坏仍然是一个谜。 根据最近的观察，深度约75-300公里的地震经常沿着近水平断层发生，我们开发了新的假设和测试来调查这些断层的优势和原因。 当板块弯曲和俯冲时，外部隆起断层是否仍然很弱？ 或者，是化石外隆断层强大，因为他们已经愈合？ 弯曲板块中的应力场是否导致向下抽水引发地震？ 是否存在持续的断层带？ 破裂扩展是等压过程吗？ 不同的地震观测将支持或反驳这些假设中的每一个，我们选择了两个研究区域，日本和哥伦比亚，其特征和区域数据集非常适合回答这些问题。 在日本，我们正在使用宽带F-Net记录来分析~500次地震的方向性，这些地震的震级低至~4.5级。 在哥伦比亚，我们正在与安第斯山脉大学的German Prieto教授合作，通过重新定位和震源特征分析考卡2000年左右的地震群。 这些分析将促进对地球科学中一个长期悬而未决的问题的理解。 在这个过程中，研究生，本科生和早期职业科学家的参与将促进教学和培训，国际合作将加强研究和教育的基础设施。