Regierungspraesidium Freiburg - Dept. … |
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GeORG Temperature Data
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- GeORG, Temperature data, Geothermal energy
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Regierungspraesidium Freiburg - Dept. 9 State Authority for Geology, Mineral Resources and Mining (unverified)
Contact information:
Guenter Sokol
Regierungspraesidium Freiburg - Dept. 9 State Authority for Geology, Mineral Resources and Mining
POSTAL:
Regierungspräsidium Freiburg - Abteilung 9 Landesamt für Geologie, Rohstoffe und Bergbau, Albertstraße 5, D-79104 Freiburg i. Br., D-79104 Freiburg i. Br., GermanyEmail:
Phone: +49 (0)761-208-3000
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Interreg IV project "GeORG": Temperature maps with different themes: Temperature maps in 500 m steps
Available map layers (116)
GeORG Temperature Data (lgrb_georg_temp_en)
Interreg IV project "GeORG": Temperature maps with different themes: Temperature maps in 500 m steps
Temperature at depth of 500 m below surface (g_temp500n)
The map shows the temperature distribution (degree Celsius) in 500 m below surface in the inner project area. Colours are similar for all maps of this kind and are therefore comparable. The model accuracy is shown in the additional map of standard deviation. The occurrency of geothermal units (simplified) plus faults and faultzones in the same depth are shown. For details see final report of INTERREG IV project "GeORG".
Temperature at depth of 500 m below surface (g_temp500g)
Geothermal units in 500 m below surface (g_geounit500f)
Faults in 500 m below surface (g_tec500l)
Temperature at depth of 1000 m below surface (g_temp1000n)
The map shows the temperature distribution (degree Celsius) in 1000 m below surface in the inner project area. Colours are similar for all maps of this kind and are therefore comparable. The model accuracy is shown in the additional map of standard deviation. The occurrency of geothermal units (simplified) plus faults and faultzones in the same depth are shown. For details see final report of INTERREG IV project "GeORG".
Temperature at depth of 1000 m below surface (g_temp1000g)
Geothermal units in 1000 m below surface (g_geounit1000f)
Faults in 1000 m below surface (g_tec1000l)
Temperature at depth of 1500 m below surface (g_temp1500n)
The map shows the temperature distribution (degree Celsius) in 1500 m below surface in the inner project area. Colours are similar for all maps of this kind and are therefore comparable. The model accuracy is shown in the additional map of standard deviation. The occurrency of geothermal units (simplified) plus faults and faultzones in the same depth are shown. For details see final report of INTERREG IV project "GeORG".
Temperature at depth of 1500 m below surface (g_temp1500g)
Geothermal units in 1500 m below surface (g_geounit1500f)
Faults in 1500 m below surface (g_tec1500l)
Temperature at depth of 2000 m below surface (g_temp2000n)
The map shows the temperature distribution (degree Celsius) in 2000 m below surface in the inner project area. Colours are similar for all maps of this kind and are therefore comparable. The model accuracy is shown in the additional map of standard deviation. The occurrency of geothermal units (simplified) plus faults and faultzones in the same depth are shown. For details see final report of INTERREG IV project "GeORG".
Temperature at depth of 2000 m below surface (g_temp2000g)
Geothermal units in 2000 m below surface (g_geounit2000f)
Faults in 2000 m below surface (g_tec2000l)
Temperature at depth of 2500 m below surface (g_temp2500n)
The map shows the temperature distribution (degree Celsius) in 2500 m below surface in the inner project area. Colours are similar for all maps of this kind and are therefore comparable. The model accuracy is shown in the additional map of standard deviation. The occurrency of geothermal units (simplified) plus faults and faultzones in the same depth are shown. For details see final report of INTERREG IV project "GeORG".
Temperature at depth of 2500 m below surface (g_temp2500g)
Geothermal units in 2500 m below surface (g_geounit2500f)
Faults in 2500 m below surface (g_tec2500l)
Temperature at depth of 3000 m below surface (g_temp3000n)
The map shows the temperature distribution (degree Celsius) in 3000 m below surface in the inner project area. Colours are similar for all maps of this kind and are therefore comparable. The model accuracy is shown in the additional map of standard deviation. The occurrency of geothermal units (simplified) plus faults and faultzones in the same depth are shown. For details see final report of INTERREG IV project "GeORG".
Temperature at depth of 3000 m below surface (g_temp3000g)
Geothermal units in 3000 m below surface (g_geounit3000f)
Faults in 3000 m below surface (g_tec3000l)
Estimation of potential for geothermal ocupandy based on temperature in 500 m below surface (g_temp500nk)
The map shows the estimation of potential for geothermal ocupandy based on temperature distribution (degree Celsius) in 500 m below surface for the inner project area. In addition, faults and fault zones in the same depth are shown. For details see final report of INTERREG IV project "GeORG".
Temperatures required for geothermal use in 500 m below surface (g_temp500g_k)
Faults in 500 m below surface (g_tec500l-1)
Estimation of potential for geothermal ocupandy based on temperature in 1000 m below surface (g_temp1000nk)
The map shows the estimation of potential for geothermal ocupandy based on temperature distribution (degree Celsius) in 1000 m below surface for the inner project area. In addition, faults and fault zones in the same depth are shown. For details see final report of INTERREG IV project "GeORG".
Temperatures required for geothermal use in 1000 m below surface (g_temp1000g_k)
Faults in 1000 m below surface (g_tec1000l-1)
Estimation of potential for geothermal ocupandy based on temperature in 1500 m below surface (g_temp1500nk)
The map shows the estimation of potential for geothermal ocupandy based on temperature distribution (degree Celsius) in 1500 m below surface for the inner project area. In addition, faults and fault zones in the same depth are shown. For details see final report of INTERREG IV project "GeORG".
Temperatures required for geothermal use in 1500 m below surface (g_temp1500g_k)
Faults in 1500 m below surface (g_tec1500l-1)
Estimation of potential for geothermal ocupandy based on temperature in 2000 m below surface (g_temp2000nk)
The map shows the estimation of potential for geothermal ocupandy based on temperature distribution (degree Celsius) in 2000 m below surface for the inner project area. In addition, faults and fault zones in the same depth are shown. For details see final report of INTERREG IV project "GeORG".
Temperatures required for geothermal use in 2000 m below surface (g_temp2000g_k)
Faults in 2000 m below surface (g_tec2000l-1)
Estimation of potential for geothermal ocupandy based on temperature in 2500 m below surface (g_temp2500nk)
The map shows the estimation of potential for geothermal ocupandy based on temperature distribution (degree Celsius) in 2500 m below surface for the inner project area. In addition, faults and fault zones in the same depth are shown. For details see final report of INTERREG IV project "GeORG".
Temperatures required for geothermal use in 2500 m below surface (g_temp2500g_k)
Faults in 2500 m below surface (g_tec2500l-1)
Estimation of potential for geothermal ocupandy based on temperature in 3000 m below surface (g_temp3000nk)
The map shows the estimation of potential for geothermal ocupandy based on temperature distribution (degree Celsius) in 3000 m below surface for the inner project area. In addition, faults and fault zones in the same depth are shown. For details see final report of INTERREG IV project "GeORG".
Temperatures required for geothermal use in 3000 m below surface (g_temp3000g_k)
Faults in 3000 m below surface (g_tec3000l-1)
Depth of 60°C isotherm (g_temp60i)
The map shows the depth of the 60 °C-isotherm in the inner project area. Colours are similar for all maps of this kind and are therefore comparable. The model accuracy is shown in the additional map of standard deviation. In addition, faults and faultzones in the same depth are shown. For details see final report of INTERREG IV project "GeORG".
60°-Isotherme (g_temp60dg)
Faults at 60°C-Isotherme (g_tec60dl)
Depth of 100°C isotherm (g_temp100i)
The map shows the depth of the 100 °C-isotherm in the inner project area. Colours are similar for all maps of this kind and are therefore comparable. The model accuracy is shown in the additional map of standard deviation. In addition, faults and faultzones in the same depth are shown. For details see final report of INTERREG IV project "GeORG".
100°-Isotherme (g_temp100dg)
Faults at 100°C-Isotherme (g_tec100dl)
Depth of 150°C isotherm (g_temp150i)
The map shows the depth of the 150 °C-isotherm in the inner project area. Colours are similar for all maps of this kind and are therefore comparable. The model accuracy is shown in the additional map of standard deviation. In addition, faults and faultzones in the same depth are shown. For details see final report of INTERREG IV project "GeORG".
150°-Isotherme (g_temp150dg)
Faults at 150°C-Isotherme (g_tec150dl)
Geology at 60°C isotherm (g_temp60g)
The map shows the geology at the 60 °C-isotherm in the inner project area. Faults and faultzones are not shown. For details see final report of INTERREG IV project "GeORG".
Geology at 100°C isotherm (g_temp100g)
The map shows the geology at the 100 °C-isotherm in the inner project area. Faults and faultzones are not shown. For details see final report of INTERREG IV project "GeORG".
Geology at 150°C isotherm (g_temp150g)
The map shows the geology at the 150 °C-isotherm in the inner project area. Faults and faultzones are not shown. For details see final report of INTERREG IV project "GeORG".
Temperature at top Malm (g_temptjot)
The map shows the temperature distribution (degree Celsius) at top Malm for the inner project area. Colours are similar for all maps of this kind and are therefore comparable. The model accuracy is shown in the additional map of standard deviation. Faults and fault zones in the same depth are also shown. For details see final report of INTERREG IV project "GeORG".
Temperature top malm [°C] (g_temptjog)
Occurence top malm (g_vgtjof)
Fault top malm (g_tectjof)
Faults top malm (g_tectjol)
Estimation of potential for geothermal ocupandy based on temperature at top Malm (g_temptjotk)
The map shows the temperature distribution (degree Celsius) at top Malm for the inner project area. The classification follows generally accepted limits of technical and economic boundaries for geothermal use. In addition, the depth of top Malm (m below surface) is shown with isolines. The model accuracy is shown in the additional map of standard deviation. Faults and fault zones in the same depth are also shown. For details see final report of INTERREG IV project "GeORG".
Temperatures required for geothermal use (g_temptjog-1)
Occurence malm (g_vgtjof-1)
Fault zone top malm (g_tectjof-1)
Faults top malm (g_tectjol-1)
Temperature at top Main Oolite (g_tempthrt)
The map shows the temperature distribution (degree Celsius) at top Main Oolite for the inner project area. Colours are similar for all maps of this kind and are therefore comparable. The model accuracy is shown in the additional map of standard deviation. Faults and fault zones in the same depth are also shown. For details see final report of INTERREG IV project "GeORG".
Temperature top main oolite [°C] (g_tempthrg)
Occurence top main oolite (g_vgthrf)
Fault top main oolite (g_tecthrf)
Faults top main oolite (g_tecthrl)
Estimation of potential for geothermal ocupandy based on temperature at top Main Oolite (g_tempthrtk)
The map shows the temperature distribution (degree Celsius) at top Main Oolite for the inner project area. The classification follows generally accepted limits of technical and economic boundaries for geothermal use. In addition, the depth of top Main Oolite (m below surface) is shown with isolines. The model accuracy is shown in the additional map of standard deviation. Faults and fault zones in the same depth are also shown. For details see final report of INTERREG IV project "GeORG".
Temperatures required for geothermal use at top main oolite (g_tempthrg-1)
Occurence Main Oolite (g_vgthrf-1)
Fault zone (g_tecthrf-1)
Faults top main oolite (g_tecthrl-1)
Temperature at top Upper Muschelkalk (g_temptmot)
The map shows the temperature distribution (degree Celsius) at top Upper Muschelkalk for the inner project area. Colours are similar for all maps of this kind and are therefore comparable. The model accuracy is shown in the additional map of standard deviation. Faults and fault zones in the same depth are also shown. For details see final report of INTERREG IV project "GeORG".
Temperature top upper muschelkalk [°C] (g_temptmog)
Occurence top upper muschelkalk (g_vgtmof)
Fault top upper muschelkalk (g_tectmof)
Faults top upper muschelkalk (g_tectmol)
Estimation of potential for geothermal ocupandy based on temperature at top Upper Muschelkalk (g_temptmotk)
The map shows the temperature distribution (degree Celsius) at top Upper Muschelkalk for the inner project area. The classification follows generally accepted limits of technical and economic boundaries for geothermal use. In addition, the depth of top Upper Muschelkalk (m below surface) is shown with isolines. The model accuracy is shown in the additional map of standard deviation. Faults and fault zones in the same depth are also shown. For details see final report of INTERREG IV project "GeORG".
Temperatures required for geothermal use at top upper muschelkalk (g_temptmog-1)
Occurence upper muschelkalk (g_vgtmof-1)
Fault zone top upper muschelkalk (g_tectmof-1)
Faults top upper muschelkalk (g_tectmol-1)
Temperature at Top Buntsandstein (g_temptst)
The map shows the temperature distribution (degree Celsius) at top Permo-Triassic sandstones for the inner project area. Colours are similar for all maps of this kind and are therefore comparable. The model accuracy is shown in the additional map of standard deviation. Faults and fault zones in the same depth are also shown. For details see final report of INTERREG IV project "GeORG".
Temperature top Buntsandstein [°C] (g_temptsg)
Occurence top Buntsandstein (g_vgtsf)
Fault top Buntsandstein (g_tectsf)
Faults top Buntsandstein (g_tectsl)
Estimation of potential for geothermal ocupandy based on temperature at top Buntsandstein (g_temptstk)
The map shows the temperature distribution (degree Celsius) at top Permo-Triassic sandstones for the inner project area. The classification follows generally accepted limits of technical and economic boundaries for geothermal use. In addition, the depth of top Permo-Triassic sandstones (m below surface) is shown with isolines. The model accuracy is shown in the additional map of standard deviation. Faults and fault zones in the same depth are also shown. For details see final report of INTERREG IV project "GeORG".
Temperatures required for geothermal use at top Buntsandstein (g_temptsg-1)
Occurence Buntsandstein (g_vgtsf-1)
Fault zone Buntsandstein (g_tectsf-1)
Faults top Buntsandstein (g_tectsl-1)
Temperature at top Permo-Carboniferous (g_temptrcot)
The map shows the temperature distribution (degree Celsius) at top Permo-Carboniferous for the inner project area. Colours are similar for all maps of this kind and are therefore comparable. The model accuracy is shown in the additional map of standard deviation. Faults and fault zones in the same depth are also shown. For details see final report of INTERREG IV project "GeORG".
Temperature top Permo-Carboniferous [°C] (g_temptrcog)
Occurence top Permo-Carboniferous (g_vgrcof)
Fault top Permo-Carboniferous (g_tectrcof)
Faults top Permo-Carboniferous (g_tectrcol)
Estimation of potential for geothermal ocupandy based on temperature at top Permo-Carboniferous (g_temptrcotk)
The map shows the temperature distribution (degree Celsius) at top Permo-Carboniferousfor the inner project area. The classification follows generally accepted limits of technical and economic boundaries for geothermal use. In addition, the depth of top Permo-Triassic sandstones (m below surface) is shown with isolines. The model accuracy is shown in the additional map of standard deviation. Faults and fault zones in the same depth are also shown. For details see final report of INTERREG IV project "GeORG".
Temperatures required for geothermal use at top Permo-Carboniferous (g_temptrcog-1)
Occurence Permo-Carboniferous (g_vgrcof-1)
Fault zone top Permo-Carboniferous (g_tectrcof-1)
Faults top Permo-Carboniferous (g_tectrcol-1)
Temperature at top Basement rocks (g_temptkrt)
The map shows the temperature distribution (degree Celsius) at top Basement rocks for the inner project area. Colours are similar for all maps of this kind and are therefore comparable. The model accuracy is shown in the additional map of standard deviation. Faults and fault zones in the same depth are also shown. For details see final report of INTERREG IV project "GeORG".
Temperature top basement rocks [°C] (g_temptkrg)
Occurence top basement rocks (g_vgtkrf)
Fault top basement rocks (g_tectkrf)
Faults top basement rocks (g_tectkrl)
Estimation of potential for geothermal ocupandy based on temperature at top Basement rocks (g_temptkrtk)
The map shows the temperature distribution (degree Celsius) at top Basement rocks for the inner project area. The classification follows generally accepted limits of technical and economic boundaries for geothermal use. In addition, the depth of top Basement rocks (m below surface) is shown with isolines. The model accuracy is shown in the additional map of standard deviation. Faults and fault zones in the same depth are also shown. For details see final report of INTERREG IV project "GeORG".
Temperatures required for geothermal use at top basement rocks (g_temptkrg-1)
Occurence basement rocks (g_vgtkrf-1)
Fault zone basement rocks (g_tectkrf-1)
Faults top basement rocks (g_tectkrl-1)
Isolines basement rock (g_postkrl)
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