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Abstract: Rate-state friction is insufficient to explain co and interseismic deformation associated with repeated caldera collapse earthquakes (AGU25)

Rate-state friction is insufficient to explain co and interseismic deformation associated with repeated caldera collapse earthquakes

Rebeca Ursu, Stanford University, Department of Geophysics, Stanford, United States, Josh Crozier, U.S. Geological Survey - California Volcano Observatory, Moffet Field, United States and Paul Segall, Stanford University, Department of Geophysics, Stanford, CA, United States
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