TY  - JOUR
A1  - Zhao, Peng
A1  - Kuhn, Daniela
A1  - Oye, Volker
A1  - Cesca, Simone
T1  - Evidence for tensile faulting deduced from full waveform moment tensor inversion during the stimulation of the Basel enhanced geothermal system
JF  - Geothermics : an international journal of geothermal research and its applications
N2  - Our study presents the results of a moment tensor inversion of 19 microseismic events with M-L between 2.0 and 3.4, associated with the stimulation operation of an enhanced geothermal reservoir in Basel, Switzerland, in 2006. We adopt a three-step procedure to retrieve point source solution parameters based on full waveform inversion. The inversion is performed by fitting displacement amplitude spectra and displacement seismograms in the first and second step, respectively, assuming a double couple source model and thus obtaining focal solutions for all 19 events. Our results are in agreement with focal mechanisms from a previous study, which employed P wave first-motion polarities from more than 40 stations, whereas our solutions are achieved using full waveform data recorded by less than 10 surface stations. In the last step, a full moment tensor inversion is performed. The results from the moment tensor inversion show an improvement on the waveform fitting compared to the double couple models, which is verified by an F-test. We investigate the stability of the moment tensor solutions by employing different velocity models. The isotropic components of the moment tensor solutions of some events are not negligible, suggesting source volume changes due to fluid injection. Events with significant isotropic components occurred mainly during the stimulation phase and close to the injection well. On the other hand, events that occurred in the post-stimulation phase are predominantly pure shear failure and located further away from the well bore. These spatio-temporal patterns can be explained by the influence of pore pressure variations during and after the hydraulic stimulation at the geothermal site. (C) 2014 Elsevier Ltd. All rights reserved.
KW  - Induced seismicity
KW  - Hydraulic fracture
KW  - Crack opening and closure
KW  - Source mechanism
KW  - F-test
Y1  - 2014
U6  - https://doi.org/10.1016/j.geothermics.2014.01.003
SN  - 0375-6505
SN  - 1879-3576
VL  - 52
SP  - 74
EP  - 83
PB  - Elsevier
CY  - Oxford
ER  -