Physics
Scientist
Department of Geophysics, Stanford University, Stanford, California
A mechanical model of the San Andreas fault and SAFOD Pilot Hole stress measurements
A transect across the Mesozoic accretionary margin of central California
Did Earthquakes Keep the Early Crust Habitable?
Fracture permeability and in situ stress to 7 km depth in the KTB Scientific Drillhole
Regional tectonic stress near the San Andreas fault in central and southern California
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