Collaborative Research: Sedimentary signature of shallow and tsunamigenic megathrust ruptures: Observations and physical models from recent catastrophic events

合作研究：浅海和引发海啸的巨型逆冲断裂的沉积特征：最近灾难性事件的观测和物理模型

• 批准号: 2044916
• 负责人: Christopher Paola
• 金额: $ 13.5万
• 依托单位: University of Minnesota-Twin Cities
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2021
• 资助国家: 美国
• 起止时间: 2021-08-01 至 2024-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2044916&HistoricalAwards=false
• 关键词: Collaborative; Research; Sedimentary; signature; shallow

The 2004 Sumatra and the 2011 Tohoku-Oki mega-earthquakes and tsunamis were catastrophic geologic events with major societal consequences. Both produced huge ruptures in areas of subducting tectonic plate boundaries that were not expected to have such large earthquakes. The large fault displacement reached the sea-floor of oceanic trenches, causing the huge tsunamis. Plate boundaries like these are the most consequential source of submarine earthquakes, especially tsunamigenic ones, and the only source of similarly large earthquakes. These two most recent ones were particularly significant in stimulating marine research and in providing further understanding of mega-earthquakes and associated tsunamis. Data on earlier large events are critical to addressing where and how often such events occur and what to expect from them, but few such events are available with instrumental data. The only recourse is reconstruction of older mega-earthquakes from their record in sediment deposits. Pioneering deep-water research in submarine earthquake geology is now using the sedimentary signature of the Tohoku-Oki earthquake to recognize signatures of previous large earthquakes. This research is advancing our understanding about the unique characteristics of sedimentation events associated with exceptionally large earthquakes and helping to distinguish them in the sedimentary record. Typical event deposits include laminated, chaotic, and homogeneous sediments (“homogenites”). This study will combine field observations, including deposits and documentation of widespread surface sediment mobilization, with a novel laboratory “sediment shaker”, to better understand the unique attributes of these rare but devastating events. The project supports the training of students and an early career scientist.The largest megathrust earthquakes at subduction margins remobilize sediment over ruptures 100s of km wide, leaving characteristic event-deposits in the stratigraphy. They generally include an acoustically transparent layer that is lithlogically, physically and geochemically homogeneous (“homogenite”), plus acoustically laminated layers with a wide range of sedimentary structures and composition (“turbidites”). The muddy homogenites from the 2011 Japan earthquake have been recently discovered to derive from widespread remobilization of surficial (few cm) sediment, while sand-rich turbidites are thought to derive from slope failures and diverse sources. This difference holds for other earthquakes and settings, suggesting distinct remobilization processes. This hypothesis will be tested by laboratory experiments that will explore whether these processes respond to different parts of the earthquake spectrum. Another question to be addressed is whether the exceptionally large and sustained long-period oscillations of the sea floor above M≥9.0 megathrust ruptures can entrain surficial sediment and thus account for the homogenites. Exceptional data sets from the 2011 Tohoku earthquake will be available to conduct the experiments. Through collaborations, samples from the Cascadia Margin, Lesser Antilles and Balearic Abyssal plain will be added. The comparisons of global observations from geophysical and core data with the physical experiments, will provide a major step forward in understanding the ways in which earthquakes remobilize sediments and advances the field of submarine paleoseismology to recognize megaquake event deposits.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.

2004年苏门答腊和2011年东北-隐岐特大地震和海啸是灾难性的地质事件，具有重大的社会后果。两者都在俯冲构造板块边界地区产生了巨大的断裂，这些地区预计不会发生如此大的地震。巨大的断层位移到达了海沟的海底，引起了巨大的海啸。 像这样的板块边界是海底地震，特别是海啸的最重要来源，也是类似大地震的唯一来源。最近的这两次活动在促进海洋研究和进一步了解特大地震及相关海啸方面特别重要。关于早期大型事件的数据对于确定此类事件发生的地点和频率以及对它们的预期至关重要，但此类事件很少有仪器数据。唯一的办法是根据沉积物中的记录重建更早的大地震。 在海底地震地质学的深水研究中，目前正在利用东北冲地震的沉积特征来识别以前大地震的特征。这项研究正在推进我们对与特大地震相关的沉积事件的独特特征的理解，并有助于在沉积记录中区分它们。典型的事件沉积物包括层状、无序和均质沉积物（“均质岩”）。这项研究将结合联合收割机实地观察，包括沉积和广泛的表面沉积物动员的文件，与一个新的实验室“沉积物振荡器”，以更好地了解这些罕见的，但破坏性的事件的独特属性。 该项目支持培训学生和一名早期职业科学家。俯冲边缘最大的巨型逆冲断层地震使沉积物重新移动到数百公里宽的断裂上，在地层中留下特有的事件沉积物。它们一般包括一个在岩石学、物理学和地球化学上均质的透声层（“均质岩”），加上具有各种沉积结构和成分的声学层压层（“浊积岩”）。最近发现，2011年日本地震的泥质均质岩来自表层（几厘米）沉积物的广泛再活化，而富含砂的浊积岩被认为来自边坡破坏和多种来源。这种差异适用于其他地震和背景，表明不同的再活化过程。这一假设将通过实验室实验来检验，这些实验将探索这些过程是否对地震谱的不同部分作出反应。另一个需要解决的问题是，M≥9.0的巨型逆冲断裂之上的海底异常巨大和持续的长周期振荡是否能够夹带表层沉积物，从而解释均质岩的形成。2011年东北地震的特殊数据集将可用于进行实验。通过合作，将增加来自卡斯卡迪亚边缘、小安的列斯群岛和巴利阿里深海平原的样本。通过对地球物理和岩心数据的全球观测与物理实验进行比较，将在理解地震重新活化沉积物的方式方面向前迈出重要一步，并推动海底古地震学领域认识特大地震事件沉积物。该奖项反映了NSF的法定使命，并被认为值得通过使用基金会的知识价值和更广泛的影响审查标准进行评估来支持。