Presentation Title
Global Positioning System Tracking of Slip Rates along Faults within the Bakersfield Transect
Presentation Type
Poster Presentation/Art Exihibt
College
College of Natural Sciences
Major
Geological Sciences
Location
Event Center BC
Start Date
5-18-2017 11:00 AM
End Date
5-18-2017 12:00 PM
Abstract
The purpose of this study was to estimate fault slip rates faults within a transect crossing the Pacific-North American plate boundary near Bakersfield, California, by inputting a set of geodetic data into an elastic model. The San Andreas Fault (SAF) slip rate estimated in this study ranges from a high of 34 mm/ yr to a low of 30 mm/yr. The value obtained for SAF in the best-fitting model is 32 mm/yr. Owens Valley Fault is slipping at 2 mm/yr. The Hosgri Fault yielded a slip rate of 2 mm/yr. The Southern Sierra Nevada Fault is slipping at 9 mm/yr. The Hunter Mountain Fault is not slipping at all right now, and the Death Valley Fault is currently slipping at 5 mm/yr. The aforementioned slip rates yielded the lowest χ2 per degree of freedom. This information is useful because it can constrain the seismic hazard on faults in this area.
Global Positioning System Tracking of Slip Rates along Faults within the Bakersfield Transect
Event Center BC
The purpose of this study was to estimate fault slip rates faults within a transect crossing the Pacific-North American plate boundary near Bakersfield, California, by inputting a set of geodetic data into an elastic model. The San Andreas Fault (SAF) slip rate estimated in this study ranges from a high of 34 mm/ yr to a low of 30 mm/yr. The value obtained for SAF in the best-fitting model is 32 mm/yr. Owens Valley Fault is slipping at 2 mm/yr. The Hosgri Fault yielded a slip rate of 2 mm/yr. The Southern Sierra Nevada Fault is slipping at 9 mm/yr. The Hunter Mountain Fault is not slipping at all right now, and the Death Valley Fault is currently slipping at 5 mm/yr. The aforementioned slip rates yielded the lowest χ2 per degree of freedom. This information is useful because it can constrain the seismic hazard on faults in this area.