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Arkosic Rocks From the San Andreas Fault Observatory at Depth (SAFOD) Borehole, Central California: Implications for the Structure and Tectonics of the San Andreas Fault Zone
The San Andreas Fault Observatory at Depth (SAFOD) drill hole encountered indurated, high-seismic-velocity arkosic sedimentary rocks west of the active trace of the San Andreas fault in central California. The arkosic rocks are juxtaposed against granitic rocks of the Salinian block to the southwest
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