Collaborative Research: Towards an Understanding of the Collective Behavior of Regional Fault Networks: The Marlborough Fault System, New Zealand

合作研究：了解区域断层网络的集体行为：新西兰马尔堡断层系统

• 批准号: 1321914
• 负责人: James Dolan
• 金额: $ 35.96万
• 依托单位: University of Southern California
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2013
• 资助国家: 美国
• 起止时间: 2013-08-01 至 2018-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1321914&HistoricalAwards=false
• 关键词: Collaborative; Research; Towards; Understanding; Collective

The primary goal of this project is to determine how different faults in regional fault networks interact with one another to accommodate the relative motion of tectonic plates over time scales ranging from one to a few dozen earthquakes. The research team will focus on a particularly promising study area in northern South Island, New Zealand, where relative motions between the Pacific and Australian plates are partitioned amongst a set of four, parallel strike-slip faults known as the Marlborough fault system. Historical and paleo-earthquake data from the Marlborough fault system, which provides a useful analog for similar fault system elsewhere in the world (e.g., northern and southern California, Northwest Turkey, Hispaniola, parts of central and Southeast Asia, Iran-Pakistan), reveal tantalizing hints of complex earthquake occurrence, with possible temporal and spatial clustering of earthquakes that varies from cycle to cycle. But currently there are too few fault slip rate and paleo-earthquake age and displacement data to fully assess the collective spatial-temporal behavior of the Marlborough fault system. In order to document in detail how the four Marlborough faults share the tectonic plate motions, the research team will determine the rates of slip along each of these faults at a variety of time scales, ranging from a few to a few dozen earthquakes, as well as the ages and displacements of past earthquakes. Key to this effort will be the acquisition of about 300 square kilometers of high-resolution lidar digital topographic data from the four main Marlborough fault system faults. These data allow the efficiently mapping and measurement in unprecedented detail of fault offsets ranging from about 100 meters down to the smallest offsets that occurred in the most recent earthquakes. The Marlborough fault system is a particularly target-rich environment in this regard because many of the large fault-crossing rivers in the Marlborough region exhibit suites of river terrace edges that have been offset by variable amounts. Combining these offset features with age data from different geochronometers (radiocarbon and optically stimulated luminescence) will yield exceptionally detailed fault slip rates at a range of time scales from individual ruptures back though several dozen earthquakes. The researchers will also excavate trenches across the four faults to determine paleo-earthquake ages and displacements, allowing cross-correlation with the youngest slip rates. The resulting data, together with existing data and the results of ongoing studies by other groups, will allow documentation of the behavior of the Marlborough faults over a wide range of temporal and spatial scales, providing the information necessary for systematic comparison with the earthquake behavior of similar systems elsewhere in the world.The primary aim of this project is to advance understanding of the way regional networks of large faults store and release seismic energy, with a particular focus on determining the relative importance of so-called emergent phenomena such as clusters of large-magnitude earthquakes and periods of transiently elevated storage of seismic energy that may not be expected in the current understanding of earthquake physics and that are not accounted for in current seismic assessment strategies. The results will help the seismic hazard community to understand how regional fault networks distribute deformation in time and space - the keys to developing more accurate, next-generation seismic hazard assessment strategies, as well as the basis for future modeling efforts aimed at understanding the causes of such phenomena. This international effort will expand already strong scientific collaboration between the US researchers and their New Zealand collaborators, benefitting both groups by fostering increased interaction between the groups, both of which face similar seismic hazards in their respective countries. Specifically, in addition to working closely with seismic hazard planners at the US Geological Survey to ensure timely implementation of their results, the PIs are actively collaborating with colleagues at GNS Science, which is responsible for implementation of seismic hazard assessment in New Zealand, ensuring that the results of this project will be also incorporated into New Zealand's next-phase seismic hazard assessments.

该项目的主要目标是确定区域断层网络中的不同断层如何相互作用，以适应构造板块在一次到几十次地震的时间尺度上的相对运动。研究小组将重点关注新西兰南岛北部一个特别有前景的研究区域，该区域太平洋板块和澳大利亚板块之间的相对运动被划分为一组四个平行的走滑断层，称为马尔堡断层系统。来自马尔堡断层系统的历史和古地震数据，为世界其他地方的类似断层系统（例如加利福尼亚州北部和南部、土耳其西北部、伊斯帕尼奥拉岛、中亚和东南亚部分地区、伊朗-巴基斯坦）提供了有用的模拟，揭示了复杂地震发生的诱人线索，地震可能在时间和空间上聚集，每个周期都有所不同。但目前断层滑移率、古地震年龄和位移数据太少，无法全面评估马尔堡断层系的集体时空行为。为了详细记录四个马尔堡断层如何共享板块运动，研究小组将确定在不同时间尺度（从几次地震到几十次地震）沿每个断层的滑动速率。作为过去地震的年龄和位移。这项工作的关键是从四个主要马尔堡断层系统断层获取约 300 平方公里的高分辨率激光雷达数字地形数据。这些数据可以对断层偏移进行前所未有的详细程度的有效测绘和测量，范围从大约 100 米到最近地震中发生的最小偏移。在这方面，马尔堡断层系统是一个目标特别丰富的环境，因为马尔堡地区的许多大型跨断层河流都表现出成套的河流阶地边缘，这些边缘已被不同程度的偏移。将这些偏移特征与来自不同地质计时仪（放射性碳和光激发光）的年龄数据相结合，将产生从数十次地震以来的单个破裂在一系列时间尺度上的异常详细的断层滑移率。研究人员还将在四个断层上挖掘沟渠，以确定古地震年龄和位移，从而与最年轻的滑移率进行互相关。由此产生的数据，加上现有数据和其他小组正在进行的研究结果，将能够记录马尔堡断层在广泛的时间和空间尺度上的行为，为与马尔堡断层的地震行为进行系统比较提供必要的信息。该项目的主要目的是加深对大型断层区域网络存储和释放地震能量方式的了解，特别关注确定所谓的突发现象（例如断层簇）的相对重要性。大地震和大地震时期瞬时升高的地震能量存储在当前对地震物理学的理解中可能是不可预期的，并且在当前的地震评估策略中也没有考虑到。研究结果将帮助地震灾害界了解区域断层网络如何在时间和空间上分布变形——这是开发更准确的下一代地震灾害评估策略的关键，也是未来旨在了解其原因的建模工作的基础此类现象。这项国际努力将扩大美国研究人员与其新西兰合作者之间业已强大的科学合作，通过促进两个群体之间的互动增加使两个群体受益，因为这两个群体在各自的国家都面临着类似的地震灾害。具体而言，除了与美国地质调查局的地震灾害规划人员密切合作以确保及时实施其结果外，PI 还与负责在新西兰实施地震灾害评估的 GNS Science 的同事积极合作，确保该项目的结果也将纳入新西兰下一阶段的地震灾害评估。