Seismological signals acquired at Soultz-sous-Forêts during the 2005 Stimulation episode. The waveforms were recorded by a downhole and a surface seismological network during the hydraulic stimulation of well GPK4 (https://cdgp.u-strasbg.fr/geonetwork/srv/eng/catalog.search#/metadata/SSF-GPK4). The complete description of the downhole seismological network is available (https://cdgp.u-strasbg.fr/geonetwork/srv/eng/catalog.search#/metadata/SSFS2004-Downhole_network). Last update of data: 31/01/2020

Microseismic catalogue of the surface network recorded at Rittershoffen during the field operations between 2012 and 2014. Calculated by ÉS-Géothermie. Number of events: 1348. The microseismic events were recorded during the drilling of the two wells and the hydraulic tests realized at GRT-1. No seismic event was recorded during the hydraulic tests realized at GRT-2. Time period: 29/11/2012 22:23:32 to 26/05/2014 23:43:55. The data parameters are the following: Column 1: Date Column 2: Origin time (UTC) Column 3: Easting in extended Lambert II coordinate system Column 4: Northing in extended Lambert II coordinate system Column 5: Latitude in WGS84 coordinate system * Column 6: Longitude in WGS84 coordinate system * Column 7: Depth (true vertical depth below sea level) Column 8: Local magnitude (vertical component) Column 9: Azimuth of the small uncertainty axis Column 10: Dip of the small uncertainty axis Column 11: Azimuth of the middle uncertainty axis Column 12: Dip of the middle uncertainty axis Column 13: Smallest uncertainty Column 14: Middle uncertainty Column 15: Largest uncertainty Column 16: Recorded period (0-GRT-1 drilling, 1-GRT-1 thermal stimulation, 20-GRT-1 hydraulic stimulation, 21-GRT-1 burst of seismicity and 3-GRT-2 drilling) * Latitude and longitude in the WGS84 coordinate system have been derived from easting and northing in extended Lambert II. Original data from Maurer et al., 2020 https://doi.org/10.1186/s40517-020-0155-2

Seismological signals acquired at Soultz-sous-Forêts during the 2003 Stimulation episode. The waveforms were recorded by a downhole and a surface seismological network during the hydraulic stimulation of well GPK3 (https://cdgp.u-strasbg.fr/geonetwork/srv/fre/catalog.search#/metadata/SSF-GPK3) and the circulation test betweeen GPK2 (https://cdgp.u-strasbg.fr/geonetwork/srv/fre/catalog.search#/metadata/SSF-GPK2) and GPK3. The downhole seismological network consisted of 6 stations and the surface network of 25 stations. The complete description of the downhole seismological network is available (https://cdgp.u-strasbg.fr/geonetwork/srv/fre/catalog.search#/metadata/SSFS2003-downhole_network). Up to now, there are only data for 4550 station. The complete description of the surface seismological network is available (https://cdgp.u-strasbg.fr/geonetwork/srv/fre/catalog.search#/metadata/SSFS2003-Surface_network). Last update of data: 31/01/2020

Seismological signals acquired at Soultz-sous-Forêts during the 2004 Stimulation episode. The waveforms were recorded by a downhole and a surface seismological network during the hydraulic stimulation of well GPK4 (https://cdgp.u-strasbg.fr/geonetwork/srv/eng/catalog.search#/metadata/SSF-GPK4). The complete description of the downhole seismological network is available (https://cdgp.u-strasbg.fr/geonetwork/srv/eng/catalog.search#/metadata/SSFS2004-Downhole_network). Last update of data: 31/01/2020

The microseismic monitoring at Rittershoffen began 6 months before any drilling. Four permanent stations were deployed at the surface in 2012 and completed the network of eight surface stations from the Soultz-sous-Forêts network. The permanent network is composed of one or three-components seismometers. A temporary network of 31 stations (TOPASE network) was deployed from June 2013 to November 2014 to improve the dectection and location of the seismic monitoring during the field development operations. The stations of the temporary network were three-component seismometers belonging to the Geophysical Instrument Pool Potsdam (GIPP) of the GFZ German Research Centre for Geosciences. Easting and northing in the file refer to the extended Lambert II Cartesian system. The latitude and longitude in the WGS84 coordinate system have been derived from the extended Lambert II Cartesian system. Original data from Maurer et al., 2020 https://doi.org/10.1186/s40517-020-0155-2

The surface seismological network in 2010 consists of 9 stations installed by EOST (Ecole et Observatoire des Sciences de la Terre) from the Strasbourg University. Last update of data: 03/02/2020

Temperature and pressure measurements recorded at various fixed depths at GPK1 (https://cdgp.u-strasbg.fr/geonetwork/srv/fre/catalog.search#/metadata/SSF-GPK1) well during 1993 stimulation. *Time is given in seconds *Temperature is given in °C *Pressure is given in MPa The zip file contains the 33 following files with measurements at the following periods and depths: - TQ13004: from 03/09/1993 23:04 to 04/09/1993 07:42 at 2804m - TQ13007: from 04/09/1993 09:36 to 04/09/1993 23:02 at 2805m - TQ13009: from 04/09/1993 23:03 to 05/09/1993 10:36 at 2805m - TQ13018: from 05/09/1993 16:25 to 05/09/1993 16:51 at 2804.96m - TQ13019: from 05/09/1993 18:53 to 06/09/1993 09:53 at 2804.96-2804.98m - TQ13026: from 06/09/1993 12:41 to 07/09/1993 10:37 at 2805m - TQ13029: from 07/09/1993 20:29 to 08/09/1993 06:43 at 2805m - TQ13036: from 08/09/1993 13:52 to 08/09/1993 17:14 at 2805m - TQ13037: from 08/09/1993 19:19 to 09/09/1993 08:41 at 2805m - TQ13043: from 09/09/1993 23:05 to 10/09/1993 06:41 at 2805m - TQ13049: from 10/09/1993 14:22 to 10/09/1993 17:17 at 2805m - TQ13051: from 10/09/1993 19:27 to 11/09/1993 09:22 at 2805m - TQ13057: from 11/09/1993 17:02 to 12/09/1993 06:51 at 2805m - TQ13063: from 12/09/1993 14:37 to 12/09/1993 15:06 at 2940m - TQ13066: from 12/09/1993 16:41 to 13/09/1993 08:33 at 2805m - TQ13073: from 13/09/1993 17:09 to 14/09/1993 06:55 at 2805m - TQ13079: from 14/09/1993 14:41 to 14/09/1993 15:13 at 2940m - TQ13081: from 14/09/1993 21:42 to 15/09/1993 08:46 at 2805m - TQ13088: from 15/09/1993 13:21 to 15/09/1993 17:06 at 2805m - TQ13089: from 15/09/1993 18:17 to 16/09/1993 06:45 at 2805m - TQ13100: from 18/09/1993 19:15 to 19/09/1993 12:15 at 2840m - TQ13101: from 19/09/1993 15:28 to 19/09/1993 16:13 at 2840m - TQ13103: from 19/09/1993 19:10 to 20/09/1993 16:06 at 2840.01m - TQ13105: from 20/09/1993 21:36 to 21/09/1993 08:22 at 2840m - TQ13107: from 21/09/1993 09:25 to 21/09/1993 13:36 at 3000m - TQ13113: from 11/10/1993 19:47 to 12/10/1993 13:58 at 2450.01m - TQ13118: from 12/10/1993 19:02 to 13/10/1993 13:50 at 2449.96-2449.97m - TQ13123: from 13/10/1993 17:51 to 14/10/1993 13:46 at 2450m - TQ13128: from 14/10/1993 17:42 to 15/10/1993 07:09 at 2450m - TQ13133: from 15/10/1993 10:57 to 16/10/1993 07:13 at 2450m - TQ13141: from 16/10/1993 13:01 to 16/10/1993 22:28 at 3520m - TQ13142: from 16/10/1993 22:28 to 17/10/1993 19:41 at 3520m - TQ13143: from 17/10/1993 19:41 to 18/10/1993 11:31 at 3520m More detailed information is given in the header of each file. Last update of data: 27/08/2019

Temperature logs recorded at GPK1 well (https://cdgp.u-strasbg.fr/geonetwork/srv/fre/catalog.search#/metadata/SSF-GPK1) during 1993 stimulation. *Depth is given in meters *Temperature is given in °C Date of the logs: - 03/09/1993 - 04/09/1993 - 05/09/1993 - 06/09/1993 - 07/09/1993 - 08/09/1993 (2 logs) - 09/09/1993 - 10/09/1993 (2 logs) - 11/09/1993 - 12/09/1993 (2 logs) - 13/09/1993 - 14/09/1993 (2 logs) - 15/09/1993 - 16/09/1993 - 18/09/1993 (3 logs) - 19/09/1993 - 20/09/1993 - 21/09/1993 - 11/10/1993 - 12/10/1993 - 13/10/1993 - 14/10/1993 - 15/10/1993 - 16/10/1993 - 18/10/1993 (2 logs) - 19/10/1993 More detailed information is given in the header of each file. Last update of data: 27/08/2019

The ECOGI powerplant (https://www.geothermies.fr/outils/operations/la-centrale-geothermique-de-rittershoffen-bas-rhin) is a geothermal powerplant designed by ÉS-Géothermie and located at Rittershoffen in northern Alsace, 7 km southeast of Soultz-sous-Forêts. The geothermal plant of Rittershoffen is operating since mid-2016 and produces 24 MWth of thermal power, with a production temperature of 170 °C. The geothermal heat production is directly used by a biorefinery located at Benheim. Two wells ensure the production and reinjection of the geothermal fluid. The development of the deep geothermal field took place between 2012 and 2014. Several earthquakes occurred between 2012 and 2014 during the drilling of the two wells GRT-1 and GRT-2 and some of the hydraulic tests realized on site. The induced seismicity was recorded by a permanent and a temporary seismic network. The Episode contains several datasets which you can find further down the page in "Links".

Surface seismic network used to study the Geoven Episode. The network consists of stations from several networks: Resif (https://www.resif.fr/) (FDSN code: FR), the French seismic network composed of high gain seismometers and accelerometers, French Accelerometric Network (FDSN code: RA), LRGB network (FDSN code: LE), the German network for Baden-Wuerttemberg, RaspberryShake network (FDSN code: AM) financed by the BCSF-Renass and the LabEx G-eau-thermie Profonde. Public stations from Fonroche network (ECK4 and VDH4) are included in the FR network. Data are automatically computed at request time