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Thrust Fault Geometry and Implications for Rupture Segmentation in the Western Central Valley

This study explores the complexity of thrust fault geometry beneath the Western Central Valley, focusing on implications for laterally continuous ruptures. It discusses right-stepping patterns, discrete structural segments, and en echelon steps that may act as rupture barriers. Additionally, it examines restraining stepover mechanics and their influence on rupture length, highlighting factors like thrust slip rate in relation to strike-slip rate. The findings underscore the need for updated models to account for the intricate fault-propagation folding above the Southern Midland Fault.

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Thrust Fault Geometry and Implications for Rupture Segmentation in the Western Central Valley

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  1. Thrust Fault Geometry beneath the Western Central Valley, andImplications for LaterallyContinuous RupturesJeff Unruh, FWLA

  2. Implications for Rupture Segmentation Right-stepping pattern - Discrete structural segments - En echelon steps = rupture barriers • Restraining stepovers - Rupture length limited by stepover dimensions - Thrust slip rate = f (strike - slip rate)

  3. Seismic Source Zones for the Sacramento-San Joaquin Delta William Lettis & Associates, Inc.

  4. Fault-Propagation Folding Above the Southern Midland Fault

  5. Conclusions • Blindthrustgeometrybeneaththe Central Valley is more complexthan currentlymodeled • En echelonstepsprobablylimitruptures

  6. Section D - D'

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