Climate Change Data Portal
DOI | 10.1029/2020JB019762 |
Creep Along the Central San Andreas Fault From Surface Fractures, Topographic Differencing, and InSAR | |
Scott C.; Bunds M.; Shirzaei M.; Toke N. | |
发表日期 | 2020 |
ISSN | 21699313 |
卷号 | 125期号:10 |
英文摘要 | Imaging tectonic creep along active faults is critical for measuring strain accumulation and ultimately understanding the physical processes that guide creep and the potential for seismicity. We image tectonic deformation along the central creeping section of the San Andreas Fault at the Dry Lake Valley paleoseismic site (36.468°N, 121.055°W) using three data sets with varying spatial and temporal scales: (1) an Interferometric Synthetic Aperture Radar (InSAR) velocity field with an ~100-km footprint produced from Sentinel-1 satellite imagery, (2) light detection and ranging (lidar) and structure-from-motion 3-D topographic differencing that resolves a decade of deformation over a 1-km aperture, and (3) surface fractures that formed over the 3- to 4-m wide fault zone during a drought from late 2012 to 2014. The InSAR velocity map shows that shallow deformation is localized to the San Andreas Fault. We demonstrate a novel approach for differencing airborne lidar and structure-from-motion topography that facilitates resolving deformation along and adjacent to the San Andreas Fault. The 40-m resolution topographic differencing resolves a 2.5 ± 0.2 cm/yr slip rate localized to the fault. The opening-mode fractures accommodate (Formula presented.) cm/yr of fault slip. A 90% ± 30% of the 1-km aperture deformation is accommodated over the several meter-wide surface trace of the San Andreas Fault. The extension direction inferred from the opening-mode fractures and topographic differencing is 40°–48° from the local trend of the San Andreas Fault. The localization of deformation likely reflects the well-oriented and mature fault. ©2020. American Geophysical Union. All Rights Reserved. |
英文关键词 | creep; Earthquake deformation; geodesy; high-resolution topography; InSAR; lidar |
语种 | 英语 |
来源期刊 | Journal of Geophysical Research: Solid Earth
![]() |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/187544 |
作者单位 | School of Earth and Space Exploration, Arizona State University, Tempe, AZ, United States; Department of Earth Science, Utah Valley University, Orem, UT, United States; Department of Geosciences, Virginia Tech, Blacksburg, VA, United States |
推荐引用方式 GB/T 7714 | Scott C.,Bunds M.,Shirzaei M.,et al. Creep Along the Central San Andreas Fault From Surface Fractures, Topographic Differencing, and InSAR[J],2020,125(10). |
APA | Scott C.,Bunds M.,Shirzaei M.,&Toke N..(2020).Creep Along the Central San Andreas Fault From Surface Fractures, Topographic Differencing, and InSAR.Journal of Geophysical Research: Solid Earth,125(10). |
MLA | Scott C.,et al."Creep Along the Central San Andreas Fault From Surface Fractures, Topographic Differencing, and InSAR".Journal of Geophysical Research: Solid Earth 125.10(2020). |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。