Collaborative Research: Characterizing Quaternary Fault Behavior and Surface Processes of an Active Rift: The Lake Malawi (Nyasa) Rift, East Africa

合作研究：表征第四纪断层行为和活动裂谷的表面过程：东非马拉维湖（尼亚萨）裂谷

• 批准号: 2116017
• 负责人: Christopher Scholz
• 金额: $ 76.38万
• 依托单位: Syracuse University
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2022
• 资助国家: 美国
• 起止时间: 2022-04-01 至 2025-03-31
• 项目状态: 未结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2116017&HistoricalAwards=false
• 关键词: Collaborative; Research; Characterizing; Quaternary; Fault

The earliest phases of the formation of ocean basins involve the break-up of the continents. The study of continental rifts is essential for understanding hazards and potential for natural resources. The process of rifting involves active faulting, volcanic activity and associated earthquakes, and are linked with significant hazards. Rifting also leads to the formation of basins that trap sediment and can host oil and gas deposits. A fundamental question in continental rift systems is how rifting is distributed across different fault systems and how surface processes, including changes in sediment supply, erosion and lake levels may impact fault behavior. These early phase geological structures act as recorders of the different processes, but after many years of seafloor spreading, are usually buried beneath thick packages of ocean sediment, and thus mature continental margins, and ocean basins, are difficult places to study early-rifting processes. On the other hand, active continental rifts, where continents are in the early stages of break-up, reveal exposed and/or shallow geological structures and deposits related to rifting. This study considers a part of the East African Rift Valley that is nearly fully flooded with freshwater (the Lake Malawi Rift), where very high quality and relatively low cost marine geophysical methods can be used to image the floor of the rift and its subsurface. By collecting very high resolution geophysical images and integrating with information from previous academic drilling and with numerical modeling, we will reconstruct fault geometries and slip rates over the last hundreds of thousands of years, evaluate controls on why particular faults are active, and estimate past earthquake activity. Results of the study will allow for a better understanding of how rift faults may be preserved and how they can be reactivated on passive continental margins, for instance on the East Coast of North America that was formed by the rifting of North America from Africa. In addition, this study will also provide information on how rift faults redirect flows of sediment into a rift valley and assist in understanding oil and gas occurrences in rift systems as well as the role of climate-driven surface processes that may influence faulting and earthquake activity. We will train 3 doctoral students and a post-doctoral scholar during the project. Our international team consists of both U.S. residents and East African nationals, including two of the latter matriculated at Syracuse University, and we anticipate roughly equal representation by female and male researchers on the field team. We will execute an extensive outreach program in Malawi, both at institutions of Higher Education and in secondary schools, and develop museum displays in Malawi. We will interact deeply with our Malawian scientific colleagues, and also engage with the Malawi Departments of Fisheries and Antiquities to share new data sets to key stakeholders.We will undertake a combined observational, analytical and numerical modeling study of Quaternary deformation and surface processes associated with a series of active fault zones in the active Lake Malawi Rift, in the western branch of the East African Rift System. This system is one of the largest active rifts in the world and is emblematic of an early-phase, low strain rate rift in a weakly magmatic system. We will use robust marine-type high-resolution seismic and echosounder tools to make high-fidelity observations across several different structural settings. Using new offshore observations from multibeam echosounder data and high-resolution CHIRP seismic reflection data, we will determine how recent (last 25-100 ka) deformation on intrarift faults is distributed across the rift and assess how intrarift faults have propagated along their length and then linked together over time. We will generate time-displacement profiles across a series of fault zones in different structural settings (e.g., flexural vs. border fault margin settings); generate a library of fault length-displacement relationships for the different fault systems; and use classical scaling laws to estimate records of past earthquakes over the past 100 ka. The fault displacement records will be chronologically constrained by the superbly-dated, high-resolution syn-rift stratigraphy from the Lake Malawi Drilling Program, extended from the drill cores into the new grids of CHIRP seismic reflection data. The new fault displacement histories will be compared to known high-resolution hydroclimate records to determine if changes in climate regimes modulate rift fault activity. Our numerical modeling efforts will assess the stress regimes associated with changes in water and sediment loading and erosion across the rift, which will be compared with observations. New lake floor bathymetric data will reveal how structurally-controlled sediment dispersal paths have developed in the Malawi Rift, leading to a better understanding basin-filling processes in rift-lake systems. Results from our study will provide unique new constraints on past earthquake histories and provide the basis for probabilistic seismic hazard assessments.Funding for this project is provided by NSF EAR Tectonics and Geophysics Programs.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.

海洋盆地形成的最早阶段涉及大陆的分裂。 研究大陆裂谷对于了解灾害和自然资源潜力至关重要。裂谷过程涉及活动断层、火山活动和相关地震，并与重大灾害有关。裂谷作用还导致盆地的形成，这些盆地捕获沉积物，并可以容纳石油和天然气矿床。大陆裂谷系统的一个基本问题是裂谷如何分布在不同的断层系统中，以及地表过程，包括沉积物供应，侵蚀和湖泊水位的变化如何影响断层行为。这些早期地质结构记录了不同的过程，但经过多年的海底扩张，通常被埋在厚厚的海洋沉积物之下，因此成熟的大陆边缘和海洋盆地是研究早期裂谷过程的困难场所。另一方面，活跃的大陆裂谷，即大陆处于分裂的早期阶段，揭示出与裂谷作用有关的裸露和/或浅层地质结构和矿床。 这项研究考虑了东非裂谷的一部分，几乎完全被淡水淹没（马拉维湖裂谷），在那里可以使用非常高质量和相对低成本的海洋地球物理方法来成像裂谷的底部及其地下。 通过收集非常高分辨率的地球物理图像，并与以前的学术钻探和数值模拟信息相结合，我们将重建断层几何形状和滑动率在过去几十万年，评估控制为什么特定的断层是活跃的，并估计过去的地震活动。研究结果将有助于更好地了解裂谷断层如何保存以及它们如何在被动大陆边缘重新激活，例如在北美东海岸，这是由北美从非洲裂谷形成的。此外，这项研究还将提供有关裂谷断层如何将沉积物流重定向到裂谷的信息，并有助于了解裂谷系统中的石油和天然气的出现，以及可能影响断层和地震活动的气候驱动的表面过程的作用。 项目期间将培养3名博士生和1名博士后。我们的国际团队由美国居民和东非国民组成，其中包括锡拉丘兹大学录取的两名东非国民，我们预计实地团队中的女性和男性研究人员的代表性大致相同。 我们将在马拉维的高等教育机构和中学实施广泛的外联方案，并在马拉维发展博物馆展览。 我们将与马拉维的科学同事深入互动，并与马拉维渔业和文物部门合作，向主要利益相关者分享新的数据集。我们将对东非裂谷系西部分支马拉维湖裂谷中一系列活动断层带的第四纪变形和地表过程进行综合观测、分析和数值模拟研究。 该系统是世界上最大的活动裂谷之一，是弱岩浆系统中早期低应变率裂谷的象征。我们将使用强大的海洋型高分辨率地震和回声测深仪工具，在几个不同的结构设置进行高保真观测。 使用新的海上观测多波束回声测深仪数据和高分辨率CHIRP地震反射数据，我们将确定如何最近（过去25-100 ka）变形的内部断层分布在整个裂谷和评估内部断层如何传播沿着其长度，然后连接在一起随着时间的推移。我们将在不同的构造背景下（例如，弯曲与边界断层边缘设置）;生成不同断层系统的断层长度-位移关系库;并使用经典的比例定律来估计过去100 ka的过去地震记录。 断层位移记录将受到马拉维湖钻探计划的超年代、高分辨率同裂谷地层学的时间限制，从岩心延伸到CHIRP地震反射数据的新网格。 新的断层位移历史将与已知的高分辨率水文气候记录进行比较，以确定气候状况的变化是否会调节裂谷断层活动。 我们的数值模拟工作将评估与水和沉积物负荷变化以及整个裂谷侵蚀相关的应力状态，并将其与观测结果进行比较。 新的湖底测深数据将揭示结构控制的沉积物扩散路径在马拉维裂谷的发展，从而更好地了解裂谷湖系统的盆地填充过程。 我们的研究结果将为过去的地震历史提供独特的新约束，并为概率地震危险评估提供基础。该项目的资金由NSF EAR构造和地球物理计划提供。该奖项反映了NSF的法定使命，并且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，被认为值得支持。

项目成果

Climate-driven stress changes and normal fault behavior in the Lake Malawi (Nyasa) Rift, East Africa

东非马拉维湖（尼亚萨）裂谷气候驱动的应力变化和正常断层行为

• DOI: 10.1016/j.epsl.2022.117693
• 发表时间: 2022
• 期刊: Earth and Planetary Science Letters
• 影响因子: 5.3
• 作者: Xue, Liang;Moucha, Robert;Scholz, Christopher A.
• 通讯作者: Scholz, Christopher A.