Collaborative Research: Paleoseismology of the M7.3 1915 Pleasant Valley Earthquake Ruptures

合作研究：1915 年 M7.3 普莱森特谷地震破裂的古地震学

• 批准号: 1920495
• 负责人: Caroline Meisner
• 金额: $ 4.91万
• 依托单位: Great Basin College
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2019
• 资助国家: 美国
• 起止时间: 2019-07-01 至 2022-06-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1920495&HistoricalAwards=false
• 关键词: Collaborative; Research; Paleoseismology; M7.3; 1915

This project to use geology to assess the past size and frequency of occurrence of large earthquakes on the fault that produced the magnitude 7.3 1915 Pleasant Valley earthquake in Nevada forms the underpinnings of a collaborative program of science, education and outreach. It is through the cumulative study of individual earthquakes that the research community gains observations to understand earthquake ruptures and their role in active tectonic processes. The information gained in this project will be incorporated into the National Hazard Maps designed to reduce failure of building infrastructure and lifelines and loss of life in future earthquakes. The collaboration of three institutes is designed to provide the opportunity for undergraduate and graduate students to learn methods and concepts bearing on earthquake science in the framework of an active research project, lead to the development of online and classroom materials for education and research, create links between rural Nevada college campuses and the University of Nevada, Reno. Principal investigators at two of the three participating institutions are early career female researchers.The study will consider one of the few large continental earthquakes that occurred in recent history and remove a significant void in our collective understanding of active tectonics in the Basin and Range and the Central Nevada Seismic Belt. This research will quantify the timing of past earthquakes and the average rate of slip on the fault that produced the Mw 7.3 1915 earthquake. The use of modern Accelerator Mass Spectrometry radiocarbon, Optical Stimulated Luminescence, and Terrestrial Cosmogenic dating methods in conjunction with paleoearthquake trenching investigations proposed herein will yield observations to 1) assess the northward extent to which slip rate is elevated along the Central Nevada Seismic Belt within the interior of the Basin and Range, 2) to determine whether the past history of events in Pleasant Valley exhibits repeated clustering of events that is observed in the Central Nevada Seismic Belt to the south, 3) address whether or not strands of the 1915 rupture separated by a 4 kilometer step in trace exhibited the same behavior in past earthquakes, 4) compare geologic rates of slip during the late Pleistocene as compared to modern geodesy, 5) cross-check multiple dating techniques applied to the same sediments, and 6) develop quantitative constraints on the timing of alluvial fan deposition in Pleasant Valley as a possible tool for assessing fault slip rates on adjacent range fronts exhibiting the same geomorphic and soil characteristics. In sum, there are few continental normal fault earthquake ruptures on which to gather observations bearing on the characteristics of rupture and recurrence. This study will provide the basis to compare and contrast characteristics of the 1915 ruptures to those that occurred before, both on the 1915 fault and elsewhere around the globe. The data collected will place observational bounds on conceptual models of earthquake recurrence and the physics of earthquake processes that form the underpinnings of seismic hazard analysis.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.

该项目利用地质学来评估断层上过去发生的大地震的规模和频率，该断层产生了 1915 年内华达州普莱森特谷 7.3 级地震，构成了科学、教育和外展合作计划的基础。通过对单次地震的累积研究，研究界获得了观测结果，以了解地震破裂及其在活跃构造过程中的作用。该项目中获得的信息将纳入国家灾害地图，旨在减少未来地震中建筑基础设施和生命线的故障以及人员伤亡。三个研究所的合作旨在为本科生和研究生提供机会，在活跃的研究项目框架内学习与地震科学相关的方法和概念，开发用于教育和研究的在线和课堂材料，建立联系在内华达州乡村大学校园和内华达大学里诺分校之间。三个参与机构中有两个的首席研究员是早期职业女性研究人员。这项研究将考虑近代历史上发生的为数不多的大型大陆地震之一，并消除我们对盆地和山脉活动构造的集体理解中的重大空白。内华达中部地震带。这项研究将量化过去地震的时间以及产生 1915 年 7.3 级地震的断层上的平均滑动率。使用现代加速器质谱放射性碳、光学受激发光和陆地宇宙成因测年方法，结合本文提出的古地震挖沟调查，将产生以下观测结果：1) 评估沿内华达中部地震带滑移率向北升高的程度。盆地和山脉的内部，2) 确定 Pleasant Valley 过去的事件历史是否表现出内华达中部观察到的事件的重复聚集南部的地震带，3) 探讨 1915 年由 4 公里台阶分开的断裂带是否在过去的地震中表现出相同的行为，4) 比较更新世晚期的地质滑动率与现代大地测量学， 5) 交叉检查应用于相同沉积物的多种测年技术，以及 6) 开发对 Pleasant Valley 冲积扇沉积时间的定量限制，作为评估断层滑移率的可能工具相邻的山脉前沿表现出相同的地貌和土壤特征。总之，很少有大陆正断层地震破裂可以收集有关破裂和复发特征的观测数据。这项研究将为 1915 年断层和全球其他地方发生的断裂特征与之前发生的断裂特征进行比较和对比提供基础。收集的数据将为地震复发的概念模型和地震过程的物理模型设置观测界限，这些模型构成了地震灾害分析的基础。该奖项反映了 NSF 的法定使命，并通过使用基金会的智力优势和更广泛的评估进行评估，被认为值得支持。影响审查标准。