|FDSN code||YN (2010-2022)||Network name||San Jacinto Fault Zone Experiment (SJFZ)|
|Start year||2010||Operated by||
|End year||2022||Deployment region||United States of America|
The San Jacinto fault is one of the most active branches of the San Andreas system in southern CA, and it consists of multiple segments that exhibit considerably different properties and behaviors both at the surface and at depth. As such, it provides an excellent natural laboratory for studying the mechanics, architecture and evolutionary behavior of a young evolving plate boundary. The goal of this project is to provide improved quantitative understanding of brittle and aseismic deformation processes at a rapidly deforming plate boundary, by linking high-quality in-situ geological, geodetic and seismological data from the San Jacinto fault zone with theoretical analyses. We conducted interdisciplinary observational studies of structural properties, earthquake source and geodetic deformation at various scales, as they relate to fault dynamics and the plate boundary tectonics in southern CA. Several distinct fault sections exist in the observation area with markedly different structural properties, slip-rates, earthquake behavior and locking depths. This diversity will enable us to perform comparative investigations of deformation processes and fault zone properties within a relatively small geographical area. Theoretical studies of dynamic ruptures and coupled evolution of earthquakes and fault structures will aid the interpretation of the observational results. The studies address several fundamental questions including:
How are properties of the fault zone at the surface (e.g., width, internal architecture, segmentation)correlated with those at depth, and what do the results imply with respect to fault evolution?
|Further information in publication(s)|
|Digital Object Identifier (DOI)||https://doi.org/10.7914/SN/YN_2010|
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