Effects of preexisting and evolving weaknesses on the kinematic evolution of strike-slip restraining bends in the Eastern California shear zone

该项目正在通过南加州的一项重点地质研究，促进人们对断层之间的障碍如何影响美国大地震发生的空间和时间的理解。太平洋和北美构造板块之间的断层边界直接穿过加利福尼亚州，通过地震震动、地面破裂和引发的山体滑坡，对其人口稠密和经济基础设施构成极端危险。然而，这一边界并不是由单一的断层组成的。在南加州，大约一半的断层活动发生在圣安德烈亚斯断层上，而其余的则分布在更广泛的断层系统中。大约25%的活动发生在125公里宽的加州东部剪切带上，该地区最近发生了破坏性(7级)地震，似乎处于活动的加强阶段。这种剪切带是神秘的，因为地震是通过多个断层上的同时或顺序运动产生的，这些断层跨越了原本被认为是屏障的缺口。该区域在测量的运动速度上也表现出差异，因为使用天基技术进行数十年的测量比基于地质偏移量的长期测量快2到3倍。这种差异可能是由于测量误差、未记录的变形或运动速率随时间的变化造成的。作为这些问题的结果，该地区未来的地震风险，包括主要的国防设施(例如，海军陆战队空中地面作战中心-MCAGCC)，以及未来的破裂可能如何与板块边界的其余部分(如洛杉矶附近)相互作用，甚至触发事件，还没有很好的了解。该项目通过记录复杂断层连接的演化和量化发生在莫哈韦沙漠南部主要断层之间的内部构造变形的大小，促进了人们的理解。这项工作包括使用高分辨率地形图绘制尖端地图，使用各种地质计时器测量测量的偏移量，以及测试地壳先前存在的弱点可能如何影响神秘的断层模式。最终，该项目将重建断层是如何演变和相互作用的，从而改进对南加州大地震的预测，并改进了解断层屏障如何控制地震大小的框架，该框架可以应用于整个美国。该项目还将通过基于互联网的视频宣传提高公众的科学素养，并加强STEM(科学、技术、工程和数学)工作队伍，从而造福社会。该项目正在东加州剪切带新生的走滑断层的起源和演化的背景下，测试地壳强度的概念性处理。一种概念性的观点认为强度是一个进化量，随着断层的平滑或随着分布变形导致的几何复杂性的增加而自动增加，强度可能会随着累积的位移而减少。另一种观点考虑地壳各向异性(即先前存在的构造弱点)如何影响断层阵列的初始几何和运动学。加州东部剪切带的几个特征可能与初始或演化的强度有关，如断层走向的可变性，断层段之间普遍存在显著的自相似约束弯曲，以及复杂的变形划分，这些都不能明显地与总断层滑动、年龄、方向或空间位置有关。该项目正在测试强度在断层发展中的作用，方法是记录通过12个关键的海退带(例如，引人注目但以前未被研究的Calico-Hidalgo断层跨越和相关的边界)的断层和褶皱(即整合或复杂化)的演化，并通过基岩填图将活动变形与地壳流变变化的模式进行比较。断层弯曲的运动学解释是基于高分辨率地形和新构造制图、构造分析、地球物理地下成像、记录断裂带之间的穿透应变以及使用综合第四纪年代的变形年表。该项目直接有助于理解扭压、力学各向异性对大陆变形的影响、走滑断层(包括可能形成破裂障碍并影响地震灾害的“地震门”)的分段和整合、大地测量和地质确定的滑移率、当地地震灾害和加州构造之间差异的原因。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影响审查标准进行评估，被认为值得支持。

This project is advancing understanding of how barriers between faults influence the spatial and temporal occurrence of major earthquakes in the United States via a focused geologic study in southern California. The fault boundary between the Pacific and North American tectonic plates cuts directly through California and poses extreme hazard to its dense population and economic infrastructure via earthquake shaking, ground rupture, and triggered landslides. This boundary does not consist of a single fault, however. In southern California, roughly half of the fault activity occurs along the San Andreas fault, whereas the remainder is distributed across a broader fault system. About 25% of the activity occurs along the 125-kilometer-wide Eastern California Shear Zone, which has produced recent damaging (magnitude7) earthquakes and appears to be in an intensified phase of activity. This shear zone is enigmatic, in that earthquakes are produced via simultaneous or sequential motion on multiple faults that cut across gaps which would have otherwise been expected to be barriers. The zone also exhibits discrepancy in measured rates of motion, as measurements spanning decades using space-based techniques are 2 to 3 times faster than long-term measurements based on geologic offsets. This discrepancy may result from measurement errors, undocumented deformation, or changes in motion rate through time. As a result of these problems, the future earthquake risk of the region, which includes major national defense installations (e.g. Marine Corps Air Ground Combat Center - MCAGCC), as well as how future ruptures may interact with or even trigger events along the remainder of the plate boundary (e.g. near Los Angeles), are not well understood. This project is advancing understanding by documenting the evolution of complex fault connections and quantifying the magnitude of internal tectonic deformation that occurs in-between the major faults of the southern Mojave Desert. This effort involves cutting-edge mapping using high-resolution topography, dating of measured offsets using various geochronometers, and testing of how preexisting weaknesses in the crust may be influencing enigmatic patterns of faulting. Ultimately the project will reconstruct of how faults have evolved and interacted, leading to improved forecasting of what to expect from major earthquakes in southern California as well as an improved framework for understanding how fault barriers control earthquake size that can be applied to the entire United States. This project will also benefit society by improving public scientific literacy via internet-based video outreach and strengthening the STEM (science, technology, engineering and mathematics) workforce.This project is testing conceptual treatments of crustal strength in the context of the origin and evolution of nascent strike-slip faults of the Eastern California Shear Zone. One conceptual view considers strength as an evolving quantity, which may decrease with accumulating displacement as faults smoothen or increase autogenically as geometric complexity grows due to distributed deformation. Another perspective considers how crustal anisotropy (i.e. preexisting structural weaknesses) influences the initial geometry and kinematics of fault arrays. Several characteristics of the Eastern California Shear Zone may relate to initial or evolving strength, such as variability in fault trend, a prevalence of prominent, self-similar restraining bends between fault segments, and complex deformation partitioning, none of which can be clearly related to total fault slip, age, orientation, or spatial position. This project is testing the role of strength in fault development by documenting the evolution of faulting and folding (i.e. integrating or complexifying) through twelve key transpressive zones (e.g. the remarkable but previously unstudied Calico-Hidalgo fault stepover and associated borderlands) and comparing active deformation to patterns of crustal rheological variations via bedrock mapping. Kinematic interpretation of fault bends is based on high-resolution topography and neotectonic mapping, structural analysis, geophysical subsurface imaging, documentation of penetrative strain between fault strands, and chronologies of deformation using comprehensive Quaternary dating. This project is directly contributing to understanding of transpression, the influence of mechanical anisotropy on continental deformation, segmentation and integration of strike-slip faults (including "earthquake gates," which may present barriers to rupture and influence seismic hazards), the cause of the discrepancy between geodetic and geologically determined slip rates, local earthquake hazards, and California tectonics.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.