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Imaging the nonvolcanic tremor zone beneath the San Andreas fault at Cholame, California using station-pair double-difference tomography
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文摘
A new station-pair double-difference seismic tomography method is presented. A detailed Vs model is obtained for the Cholame tremor zone for the first time. Most of the Cholame tremors are associated with low Vs anomalies. Low velocities are likely due to hydrous minerals and high-pressure pore fluids.

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