2020
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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
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GRT-2 is the second well drilled within the framework of the geothermal project ECOGI at Rittershoffen. The drilling of the well started in March 2014 and ended in July 2014. GRT-2 is a deviated well of 3196 m in length that reaches 2708 m TVD GL (true vertical depth from ground level) within the fractured granite basement. No reservoir enhancement was necessary at GRT-2. Production and circulation tests were realized from July to October 2014. The GRT-2 well is currently used as production well. It produces hot water at a temperature of 170 °C and with production flow rate of 70 L/s. Location of the GRT-2 wellhead (in WGS84): Latitude: 48.8970198° Longitude: 7.9386127°
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Focal mechanisms of seismic events, which occurred during the thermal and hydraulic stimulations, the 2013 July burst and the GRT-2 drilling. Two earthquakes per seismogenic period were considered. More information about the determination of the focal mechanisms and the selection of events is available in the article from Maurer, V. et al., 2020, Seismicity induced during the development of the Rittershoffen geothermal field, France. The data parameters are the following: Column 1: Period Column 2: Date Column 3: Time (UTC) Column 4: Easting (m) Column 5: Northing (m) Column 6: Depth (m TVD MSL) Column 7: Latitude (°) * Column 8: Longitude (°) * Column 9: Mlv Column 10: NPOL Column 11: Dip (°) Column 12: Strike (°) Column 13: Rake (°) * 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
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Seismological signals acquired during the development phase of the geothermal project at Rittershoffen. Waveforms from the permanent stations described in RITD-Surface_network (https://cdgp.u-strasbg.fr/geonetwork/srv/eng/catalog.search#/metadata/RITD-Surface_network) are provided for each event from RITD-Catalogue (https://cdgp.u-strasbg.fr/geonetwork/srv/eng/catalog.search#/metadata/RITD-Catalogue), (-30s, +90s). All the waveforms from the temporary seismic network installed in 2013 and 2014 are available on the GFZ (German Research Centre for Geosciences) data services website.
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Interval seismic velocities applied to the 3D velocity model. Vp, Vs and Vp/Vs values for each formation along GRT-1 well. Original data from Maurer et al., 2020
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GRT-1 is the first well drilled within the framework of the geothermal project ECOGI at Rittershoffen. The drilling of the well began at the end of September 2012. The well reached a final measured depth of 2580 m within the fractured granite basement at the end of December 2012. Hydraulic tests of the well were carried out from December 2012 to June 2013. The tests realized at GRT-1 allowed to increase its injectivity index by a factor five. The GRT-1 well is currently used as injection well. Location of the GRT-1 wellhead (in WGS84): Latitude: 48.8970080° Longitude: 7.9387218°
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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
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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
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Seismological signals acquired at Soultz-sous-Forêts during the 2000 Stimulation episode. The waveforms were recorded by a downhole and a surface seismological network during the hydraulic stimulation programme conducted at well GPK2 (https://cdgp.u-strasbg.fr/geonetwork/srv/eng/catalog.search#/metadata/SSF-GPK2). The downhole seismological network consisted of 5 stations and the surface network of 18 stations. The complete description of the downhole seismological network is available (https://cdgp.u-strasbg.fr/geonetwork/srv/eng/catalog.search#/metadata/SSFS2000-downhole_network). The complete description of the surface seismological network is available (https://cdgp.u-strasbg.fr/geonetwork/srv/eng/catalog.search#/metadata/SSFS2000-surface_network). Last update of data: 31/01/2020
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Before the 2003 episode, a permanent network designed to monitor the microseismic activity at Soultz-sous-Forêts was installed by EOST (Ecole et Observatoire des Sciences de la Terre) from the Strasbourg University. It consisted of nine stations, six one-component and three three-component sensors. The network was operational just before the 2003 stimulation of GPK3 (https://cdgp.u-strasbg.fr/geonetwork/srv/fre/catalog.search#/metadata/SSF-GPK3). A temporary network of fourteen seismometers (six three-component and eight one-component) was added to this permanent network. Contrary to the 2000 episode, all the fourteen stations of the temporary network were continuously recording. In addition to the network under the responsibility of EOST, a broad-band Güralp sensor was used mostly for waveform analysis. Two other accelerometers completed the surface monitoring system too. The coordinates of the stations have been obtained from RESIF (https://www.resif.fr/">https://www.resif.fr). Last update of data: 03/02/2020
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