The aim of the GeORG project (Geopotentials of the deep Upper Rhine Graben, https://www.geopotenziale.org/home/index_html) was to create a 3D model of the geological structure of the Upper Rhine Graben down to a depth of several kilometers. The project began in October 2008 and ended in December 2012. GeORG offers a complete geoscientific information base. Maps showing the deep structure and spatial distribution of geological layers and temperatures have been extracted. Geological cross-sections can be generated over the entire study area and in all directions. These show the stratigraphic position and stacking of layers in space. GeORG has created an information access platform for companies, public and private project developers and research organizations. The results are accessible to all at https://maps.geopotenziale.eu. Several products from the GeORG mapviewer around Soutz-sous-Forêts geothermal site are extracted.

The aim of the GeORG project (Geopotentials of the deep Upper Rhine Graben, https://www.geopotenziale.org/home/index_html) was to create a 3D model of the geological structure of the Upper Rhine Graben down to a depth of several kilometers. The project began in October 2008 and ended in December 2012. GeORG offers a complete geoscientific information base. Maps showing the deep structure and spatial distribution of geological layers and temperatures have been extracted. Geological cross-sections can be generated over the entire study area and in all directions. These show the stratigraphic position and stacking of layers in space. GeORG has created an information access platform for companies, public and private project developers and research organizations. The results are accessible to all at https://maps.geopotenziale.eu. Several products from the GeORG mapviewer around Rittershoffen site are extracted.

The objective of the GeORG project (Geopotentials of the deep Upper Rhine Graben, https://www.geopotenziale.org/home/index_html) was to create a 3D model of the geological structure of the Upper Rhine Graben down to several kilometers depth. It provides a comprehensive information base (thickness/depth maps, temperature maps, and geological cross-sections that can be generated across the entire area). The BRGM distributes the French part of this 3D geological model via its Cupidon repository (https://data.geoscience.fr/metadataRecord/4a58a7e3-8b71-4c69-9447-cb1c791d23a3). We cut out this model around the Rittershoffen site with a radius of approximately 10 km. Modeled lithological interfaces: 010_blg : Base of the Plio-Quaternary 040_bff : Base of the Froidefontaine Formation 050_bt :Base of the Tertiary 090_bju : Base of the Lias 100_bku : Base of the Keuper 110_tms : Top of the Saliferous Muschelkalk 120_bmu : Base of the Muschelkalk 130_btr : Base of the Triassic 170_kr :Top of the Hercynian 600_salt_diapirs : Salt diapirs faults_fr_s03: fault

The objective of the GeORG project (Geopotentials of the deep Upper Rhine Graben, https://www.geopotenziale.org/home/index_html) was to create a 3D model of the geological structure of the Upper Rhine Graben down to several kilometers depth. It provides a comprehensive information base (thickness/depth maps, temperature maps, and geological cross-sections that can be generated across the entire area). The BRGM distributes the French part of this 3D geological model via its Cupidon repository (https://data.geoscience.fr/metadataRecord/4a58a7e3-8b71-4c69-9447-cb1c791d23a3). We cut out this model around the Soultz-sous-Forêts site with a radius of approximately 10 km. Modeled lithological interfaces: 010_blg : Base of the Plio-Quaternary 040_bff : Base of the Froidefontaine Formation 050_bt :Base of the Tertiary 090_bju : Base of the Lias 100_bku : Base of the Keuper 110_tms : Top of the Saliferous Muschelkalk 120_bmu : Base of the Muschelkalk 130_btr : Base of the Triassic 170_kr :Top of the Hercynian 600_salt_diapirs : Salt diapirs faults_fr_s03: fault