Supplemental Material: Dynamic models of earthquake rupture along branch faults of the eastern San Gorgonio Pass region in California using complex fault structure
posted on 2020-04-01, 00:00authored byRoby Douilly, David D. Oglesby, Michele L. Cooke, Jennifer L. Hatch
Geosphere, April 2020, v. 16, no. 2, 474-489, doi:10.1130/GES02192.1, Supplemental Figures. Figure S1: Final slip (40 s into the simulation) for fault geometries A, B, and C for the dynamic model with constant tractions on all fault segments for a slip-weakening distance of 0.3 m and an S value of 0.3—lower-strength case (scenario U2). Figure S2: Initial shear stresses for geometries A, B, and C for a dynamic rupture model from a regional stress distribution of N10°W (left column) and N10°E (right column) respectively. Figure S3: Final slip distribution on fault geometries A, B, and C for a dynamic rupture model from a regional stress distribution of N10°W and N10°E respectively.