Collaborative Research: Comparing Deformation Rates in Wrench Borderlands from Geodetic and Geologic Data to Evaluate the Permanent and Recoverable Components

合作研究：根据大地测量和地质数据比较扳手边界的变形率，以评估永久和可恢复的组成部分

• 批准号: 0208416
• 负责人: Bernard Housen
• 金额: $ 8.55万
• 依托单位: Western Washington University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2002
• 资助国家: 美国
• 起止时间: 2002-07-01 至 2007-06-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0208416&HistoricalAwards=false
• 关键词: Collaborative; Research; Comparing; Deformation; Rates

The current velocity field associated with plate tectonic motion in western California is well characterized by geodetic measurements using Global Positioning Systems (GPS). The exact nature of what geodetic measurements record in actively deforming zones remains a significant problem, as this technique records both recoverable (elastic) and permanent (quasi-plastic) strains in wrench borderlands (blocks adjacent to major strike-slip faults). The goal of this proposal is to evaluate the relative magnitudes of the recoverable and permanent components in the deformation of wrench borderlands, by simultaneously studying two different sections of the San Andreas fault system. Creeping segment, central California: Geodetic measurements alone are generally unable to distinguish between recoverable and permanent deformation, because of the long (50 yr) interval between slip episodes on faults. In contrast, intervals between slip episodes are short (weeks to months) in the creeping central section of the San Andreas fault. By collecting geodetic data throughout the short seismic cycle in the creeping segment, the PI's will be able to evaluate the relative sizes of the recoverable and permanent components of the displacement field in the vicinity of the fault. They propose to check the estimates of currently accumulating permanent measurements against long-term averages determined from geologic and paleogmagnetic data. Prior work suggests clockwise rotation of the paleomagnetic signal of Miocene and younger sediments in the wrench borderlands. Documenting the areal extent, regional distribution, and amount of rotation throughout this area will allow them to calculate a long-term average for permanent deformation. This part of the proposal involves permanent GPS stations and monitoring, campaign-style GPS, paleomagnetism, and geologic mapping. Durmid Hill, Salton Trough, southern California: In this area, previous work has determined the amount of permanent strain. The PI's propose to complete a step-wise, three-dimensional retro-deformation of deformed sedimentary rocks. In order to convert these incremental strain data into estimates of deformation rates, one must have precise knowledge of time of deformation. In this region of excellent exposure, one aspect of deformation timing is provided by the presence of an ash layer correlated with the 0.76 Ma Bishop tuff. Additional information will result from paleomagnetic techniques that record the magnetic field during deposition. Utilizing the variety of ages of the different sedimentary layers to provide differential vertical axis rotations, The PI's can determine the timing of minor structures (e.g., joints, fractures, and small folds) by determining which units are affected. By comparing geodetic rates (which include both recoverable and permanent strain components) with geologic rates (which record only a permanent strain component) they can assess the amount of recoverable strain accumulation in this area. This part of the proposal involves geologic mapping, paleomagnetism, and campaign-style GPS. By combining the results of geological, geodetic, and paleomagnetic investigations from our two field areas, the PI's will assess the relative contribution of recoverable (elastic) and permanent (quasi-plastic) strains in wrench borderlands. Resolution of this issue has fundamental implications for earthquake mechanics, geological implications of borderland deformation, and potential slip magnitudes on major faults.

利用全球定位系统（GPS）的大地测量资料，对加州西部与板块构造运动有关的流速场进行了很好的描述。大地测量记录在活跃变形区的确切性质仍然是一个重要的问题，因为这种技术记录了扳手边界（邻近主要走滑断层的块体）的可恢复（弹性）和永久（准塑性）应变。本提案的目标是通过同时研究圣安德烈亚斯断层系统的两个不同部分，评估扳手边界变形中可恢复和永久成分的相对大小。蠕动段，加州中部：由于断层滑动事件之间的间隔很长（50年），因此，单独进行大地测量通常无法区分可恢复变形和永久变形。相比之下，在圣安德烈亚斯断层的蠕动中央部分，滑动事件之间的间隔很短（几周到几个月）。通过在蠕动段的短地震周期内收集大地测量数据，PI将能够评估断层附近位移场的可恢复和永久分量的相对大小。他们建议根据地质和古地磁数据确定的长期平均值来检查目前积累的永久测量的估计值。先前的工作表明顺时针旋转的古地磁信号的中新世和年轻的沉积物在扳手的边界。 记录整个地区的面积范围，区域分布和旋转量将使他们能够计算永久变形的长期平均值。提案的这一部分涉及永久性GPS站和监测、活动式GPS、古地磁学和地质测绘。加州南部索尔顿海槽的杜米德山：在这个地区，以前的工作已经确定了永久应变的数量。PI的建议，以完成一个逐步的，三维逆变形的沉积岩。为了将这些增量应变数据转换为变形速率的估计，必须对变形时间有精确的了解。在这一地区的优秀曝光，变形定时的一个方面是提供了一个灰层与0.76马毕晓普凝灰岩的存在。其他信息将来自于记录沉积过程中磁场的古地磁技术。利用不同沉积层的各种年龄来提供不同的垂直轴旋转，PI可以确定小结构（例如，节理、裂缝和小褶皱）。通过比较大地测量速率（包括可恢复和永久应变分量）与地质速率（仅记录永久应变分量），他们可以评估该地区可恢复应变累积量。这一部分的提案涉及地质测绘、古地磁学和北斗式GPS。通过结合我们两个领域的地质，大地测量和古地磁调查的结果，PI的将评估可恢复（弹性）和永久（准塑性）应变在扳手边界的相对贡献。这一问题的解决对地震力学、边界变形的地质意义和主要断层的潜在滑动幅度具有根本意义。