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Title: Steep-dip seismic imaging of the shallow San Andreas fault near Parkfield. Author: Hole JA, Catchings RD, St Clair KC, Rymer MJ, Okaya DA, Carney BJ. Journal: Science; 2001 Nov 16; 294(5546):1513-5. PubMed ID: 11711672. Abstract: Seismic reflection and refraction images illuminate the San Andreas Fault to a depth of 1 kilometer. The prestack depth-migrated reflection image contains near-vertical reflections aligned with the active fault trace. The fault is vertical in the upper 0.5 kilometer, then dips about 70 degrees to the southwest to at least 1 kilometer subsurface. This dip reconciles the difference between the computed locations of earthquakes and the surface fault trace. The seismic velocity cross section shows strong lateral variations. Relatively low velocity (10 to 30%), high electrical conductivity, and low density indicate a 1-kilometer-wide vertical wedge of porous sediment or fractured rock immediately southwest of the active fault trace.[Abstract] [Full Text] [Related] [New Search]