Collaborative Research: Reconciling Geologic and Geodetic Rates of Deformation: The Role of Distributed Strain in the Upper Crust

了解地表形变在不同时间尺度上的时空分布，可以深入了解岩石圈流变学、破裂行为和沿着断层网络的滑动传递性质。然而，全球定位系统提供的新见解带来了新的挑战：特别是，在大地测量时间尺度（小于10年）上测量的弹性应变积累与在更长时间尺度（10，000 - 1，000，000年）上推断的地质滑动之间的关系如何？在过去的几年里，许多努力都集中在地表变形的大地测量速率和横跨东加州剪切带的断层滑动的地质速率之间的明显差异。最近的假设，这种差异集中在应变场的时间变化，这是由于：1）地震应变释放的集群，2）共轭断层系统上的振荡应变释放，或3）粘弹性变形后，最近的地震。然而，为了充分了解断层系统行为变化的速度和克里思，需要对地质时期断层滑动进行完整的表征。该研究小组正在收集必要的基本地质和地貌数据，以严格评估加州欧文斯谷的断层位移速率。特别是，该项目的目的是了解小断层的扩散阵列在适应整个地区的应变所发挥的作用。这些断层网络可能是目前对大地测量数据的解释所没有考虑到的地质滑动的重要组成部分，这一假设正在通过确定分布在欧文斯谷中部和北方的许多断层阵列上的断层滑动率（利用冰川冰碛、河流阶地和冲积扇等地貌标志）进行检验。此外，另一种假设认为，地质和大地测量数据之间的差异可能反映了应变释放率的时间变化。通过利用具有不同年代的偏移标志的地点，对整个区域分布的断层的速度和克里思有了更深入的了解，该项目通过改进对北美-太平洋板块边界的大地测量数据的解释，并通过对断层滑动的时间变化问题有了新的认识，为更广泛的地质/地球物理界提出的更大目标作出了贡献。

Understanding the spatial and temporal distribution of surface deformation over various timescales can yield insight into lithospheric rheology, rupture behavior, and nature of slip transfer along fault networks. However, new insights provided by GPS bring new challenges: in particular, how does elastic strain accumulation measured over geodetic timescales (less than 10 yr) relate to geologic slip inferred over longer timescales (10,000 - 1,000,000 yr)? Over the past few years, much effort has been focused on an apparent discrepancy between geodetic rates of surface deformation and geologic rates of fault slip across the Eastern California Shear Zone. Recent hypotheses for this discrepancy center on temporal variations in the strain field which result from: 1) clustering of seismic strain release, 2) oscillatory strain release on conjugate fault systems, or 3) viscoelastic deformation following recent earthquakes. In order to fully understand the pace and tempo of variations in fault system behavior, however, a complete characterization of fault slip over geologic time is required.This investigator team is collecting the basic geologic and geomorphic data necessary to critically assess rates of fault displacement across Owens Valley, California. In particular, the project is aimed at understanding the role played by diffuse arrays of small faults in accommodating strain across the region. The hypothesis that these fault networks may account for a significant component of geologic slip not considered by current interpretations of geodetic data is being tested by determining fault slip rates (exploiting geomorphic markers such as glacial moraines, river terraces and alluvial fans) on numerous fault arrays distributed throughout central and northern Owens Valley. Moreover, an alternative hypothesis holds that the discrepancy between geologic and geodetic data may reflect temporal variation in the rate of strain release. A refined understanding of the pace and tempo of distributed faulting across the region is being developed by exploiting sites with offset markers of varying age.This project contributes towards larger goals articulated by the broader geologic/geophysical community by improving interpretations of geodetic data across the diffuse North American - Pacific plate boundary, and by developing new insight into the problem of temporal variations in fault slip.