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- W2317149009 abstract "The authors analyzed seismic events which include large events with moment magnitude larger than 2.0 observed during and after the hydraulic stimulation at Basel, Switzerland in 2006. The characteristics of the large events, including time of occurrence, hypocenter location, waveform similarity/difference to the neighboring events, fault plane solutions (FPSs), and seismic source parameters, have been investigated by the authors. We found that the characteristics of the large events, which occurred in deeper and shallower parts of the seismic cloud are different from each other. In this study, we identified orientation of fracture planes on which seismic activity was observed. Critical pore pressure for shear slip, which is considered as one of the triggers of the shear slip on existing fracture plane has been also evaluated for the large events. Many large events had fault plane solution with trend of N-S azimuth and sub-vertical dip, even the stress state of the fracture plane is not the most preferential to slip. Meanwhile, the rests of the large events including the largest one, occurred on the fracture plane with WNW-ESE azimuth trend strikes, which can be interpreted as the most preferential plane to slip in case of coefficient friction is 0.6. Such unbalanced seismic activity and release of seismic energy on fractures with different azimuths are clearly observed for this data." @default.
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- W2317149009 date "2011-01-01" @default.
- W2317149009 modified "2023-10-18" @default.
- W2317149009 title "Characteristics of the large events from the seismically activated fractures at Basel geothermal reservoir" @default.
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- W2317149009 doi "https://doi.org/10.1190/segj102011-001.29" @default.
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