The induced earthquake sequence related to the St. Gallen deep geothermal project (Switzerland): Fault reactivation and fluid interactions imaged by microseismicity

Diehl, Tobias and Kraft, Toni and Kissling, Edi and Wiemer, Stefan (2017) The induced earthquake sequence related to the St. Gallen deep geothermal project (Switzerland): Fault reactivation and fluid interactions imaged by microseismicity. Journal of Geophysical Research: Solid Earth, 122 (9). pp. 7272-7290. DOI: https://doi.org/10.1002/2017JB014473

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Official URL: http://doi.org/10.1002/2017JB014473

Abstract

In July 2013, a sequence of more than 340 earthquakes was induced by reservoir stimulations and well‐control procedures following a gas kick at a deep geothermal drilling project close to the city of St. Gallen, Switzerland. The sequence culminated in an ML 3.5 earthquake, which was felt within 10–15 km from the epicenter. High‐quality earthquake locations and 3‐D reflection seismic data acquired in the St. Gallen project provide a unique data set, which allows high‐resolution studies of earthquake triggering related to the injection of fluids into macroscopic fault zones. In this study, we present a high‐precision earthquake catalog of the induced sequence. Absolute locations are constrained by a coupled hypocenter‐velocity inversion, and subsequent double‐difference relocations image the geometry of the ML 3.5 rupture and resolve the spatiotemporal evolution of seismicity. A joint interpretation of earthquake and seismic data shows that the majority of the seismicity occurred in the pre‐Mesozoic basement, hundreds of meters below the borehole and the targeted Mesozoic sequence. We propose a hydraulic connectivity between the reactivated fault and the borehole, likely through faults mapped by seismic data. Despite the excellent quality of the seismic data, the association of seismicity with mapped faults remains ambiguous. In summary, our results document that the actual hydraulic properties of a fault system and hydraulic connections between its fault segments are complex and may not be predictable upfront. Incomplete knowledge of fault structures and stress heterogeneities within highly complex fault systems additionally challenge the degree of predictability of induced seismicity related to underground fluid injections.

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Item Type: Article
Additional Information: Supporting Information https://agupubs.onlinelibrary.wiley.com/action/downloadSupplement?doi=10.1002%2F2017JB014473&attachmentId=2172498276 https://agupubs.onlinelibrary.wiley.com/action/downloadSupplement?doi=10.1002%2F2017JB014473&attachmentId=2172498277
Subjects: Methodology > Method and procesing > Collective properties of seismicity
Methodology > Method and procesing > Technology-seismicity interaction
Region > Switzerland > St. Gallen
Inducing technology > Geothermal energy production
Project: S4CE > ST GALLEN: geothermal project