USGS · 70015412
Seismic velocities and attenuation from borehole measurements near the Parkfield prediction zone, Central California
Abstract
Shear (S)- and compressional (P)- wave velocities were measured to a depth of 195 m in a borehole near the San Andreas fault where a recurrence of a moderate Parkfield earthquake is predicted. S-wave velocities determined from orthogonal directions of the S-wave source show velocity differences of approximately 20 percent. An average shear-wave Q of 4 was determined in relatively unconsolidated sands and gravels of the Paso Robles Formation in the depth interval 57.5-102.5 m.
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James F. Gibbs, Edward F. Roth. 1989-08-01. Seismic velocities and attenuation from borehole measurements near the Parkfield prediction zone, Central California. https://doi.org/10.1193/1.1585538
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