Induced seismicity Sample Clauses

Induced seismicity. Xxxxx et al. (2017) analyzed the sequence of seismic events that occurred close to the city of St. Gallen and the related 340 events to be induced by the reservoir stimulations and well- control procedures following the gas-kick. Xxxxx et al. (2017) state that the majority of the seismicity occurred in the pre-Mesozoic basement, hundreds of meters below the borehole and the targeted Mesozoic sequence, and propose that a direct hydraulic connection exists between the borehole and the reactivated fault. It is interesting to note that a hydraulic connection from the well to the basements is postulated but no seismicity occurred along this hypothesized fluid path. The locations taken from Xxxxx et al. (2017) have been used to compare the numerical results against the induced seismicity without further questioning the correctness of the data, which is beyond the scope of this deliverable. Most of the seismic events are located on a southern fault segment of the St. Gallen Fault Zone and occurred during injection tests. They reached only very low magnitudes. The main event is also localized on the same southern fault segment.
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