T41A-2866
Seismic Reflectivity of the Crust in the Northern Salton Trough
Thursday, 17 December 2015
Poster Hall (Moscone South)
Klaus Bauer1, Gary S Fuis2, Mark Goldman2, Patricia Persaud3,4, Trond Ryberg1, Victoria E Langenheim2, Daniel S Scheirer2, Michael J Rymer2, John A Hole5, Joann M Stock3 and Rufus Catchings2, (1)GeoForschungsZentrum GFZ, Potsdam, Germany, (2)U.S. Geological Survey, Menlo Park, CA, United States, (3)California Institute of Technology, Pasadena, CA, United States, (4)California State Polytechnic University Pomona, Pomona, CA, United States, (5)Virginia Polytechnic Institute and State University, Blacksburg, VA, United States
Abstract:
The Salton Trough in southern California is a tectonically active pull-apart basin that was formed by migrating step-overs between strike-slip faults, of which the San Andreas Fault (SAF) and the Imperial Fault are the current, northernmost examples. The Salton Seismic Imaging Project (SSIP) was undertaken to improve our knowledge of fault geometry and seismic velocities within the sedimentary basins and underlying crystalline crust around the SAF. Such data are useful as input for modeling scenarios of strong ground shaking in the surrounding high-population areas. We used pre-stack depth migration of line segments from shot gathers in several seismic profiles that were acquired in the northern part of the SSIP study area (Lines 4 - 7). Our migration approach can be considered as an infinite-frequency approximation of the Fresnel volume pre-stack depth migration method. We use line segments instead of the original waveform data. We demonstrate the method using synthetic data and analyze real data from Lines 4 - 7 to illustrate the relationship between distinct phases in the time domain and their resulting image at depth. We show both normal-moveout reflections from sub-horizontal interfaces and reverse-moveout reflections from steep interfaces, such as faults. Migrated images of dipping faults, such as the SAF and the Pinto Mountain Fault, are presented in this way. The SAF is imaged along Line 4, through the Mecca Hills, as a number of steeply dipping fault segments that collectively form a flower structure, above 5 km depth, that sole into a moderately NE-dipping fault below that depth. The individual migrated reflection packages correlate with mapped surface fault traces in the Mecca Hills. A similar geometry is seen on Line 6, from Palm Springs through Yucca Valley, where fault splays sole or project into a moderately dipping SAF below 10-km depth. We also show and discuss the reflectivity pattern of the middle and lower crust for Lines 4 - 7.
