Аннотация
We determine stress drops from P-wave spectra of about 1000 earthquakes
induced by hydraulic stimulation in crystalline rock for a deep heat
mining project in Basel, Switzerland. We observe an increase in stress
drop by about a factor of five with radial distance from 10 m to
300 m, which suggests that stress drop correlates with pore pressure
perturbations due to the injection. We test this hypothesis by calculating
the injection-related pore pressure perturbation based on a simple
linear pore pressure diffusion model and find a good correlation
of the expected pore pressure perturbation with the estimated stress
drops.
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