EGDI (v1.6.16027)

« GeoERA - GeoEnergy

Base layers

Layers

All Areas

Heat-in-place (Tinj = 18 �C)

Area

Cross_section_lines

Faults

LNH

Border Folded Molasse Alps

Isolines of permeability

Isolines of permeability inferred

Transition to helvetic basin

Heat-in-place (Tinj = 18 �C)

Heat-in-place (Tinj = 50 �C)

Thickness of reservoir

Depth to top reservoir

Temperature of top reservoir

Area

Cross_section_line

Faults

Heat-in-place (Tinj = 18 �C)

Heat-in-place (Tinj = 50 �C)

Thickness of reservoir

Depth to top reservoir

Area

Cross_section_line

Faults

Heat-in-place (Tinj = 18 �C)

Thickness of reservoir

Depth to top reservoir

Temperature of top reservoir

Area

Cross_section_line

Faults

Heat-in-place (Tinj = 18 �C)

Thickness of reservoir

Depth to top reservoir

Temperature of top reservoir

Area

Cross_section_line

Faults

Heat-in-place (Tinj = 18 �C)

Heat-in-place (Tinj = 50 �C)

Thickness of reservoir

Depth to top reservoir

Temperature of top reservoir

Area

Cross_section_lines

Faults

Shallow Water Facies

Basin Facies

Heat-in-place (Tinj = 18 �C)

Heat-in-place (Tinj = 50 �C)

Thickness of reservoir

Depth to top reservoir

Temperature at top of eastern reservoir

Temperature at top of western reservoir

Area

Cross_section_line

Faults

Heat-in-place (Tinj = 18 �C)

Heat-in-place (Tinj = 50 �C)

Thickness of reservoir

Depth to top reservoir

Area

Crosssectionline

Faults

Heat-in-place (Tinj = 18 �C)

Heat-in-place (Tinj = 50 �C)

Thickness of reservoir

Depth to top reservoir

Area

Crosssectionline

Faults

Heat-in-place (Tinj = 18 �C)

Heat-in-place (Tinj = 50 �C)

Area

Cross_section_line

Fault

Heat-in-place (Tinj = 18 �C)

Heat-in-place (Tinj = 50 �C)

Thickness of reservoir

Depth to top reservoir

Temperature of top reservoir

Area

Cross_section_line

Faults

Heat-in-place (Tinj = 18 �C)

Heat-in-place (Tinj = 50 �C)

Thickness of reservoir

Depth to top reservoir

Temperature of top reservoir

Search EGDI metadata catalogue

Use this search to find WMS service entries in the EGDI Metadata Catalogue.

Add your own data (WMS)

Your WMS must support version 1.3.0. Also, it should support rather huge image dimensions - especially if the layer is not in the same projection as this map. If not, try reducing your browser window before loading the layer.

Details

« GeoERA - GeoEnergy

Layers

Overview of the HotLime Case Study Areas. Zoom in to see also the smaller areas.

Comparative depiction of the HotLime Case Studies showing the heat-in-place assessment modelled for the re-injection temperature of 18�C.

Upper Jurassic carbonates in the central part of the North Alpine Molasse Basin (DE/AT)

Click the line and follow the link to retrieve the cross-section with the reservoir rock suite color-coded in accord with International Chronostratigraphic Chart.

LNH, Landshut-Neuoetting Hoch, is a rise of the Variscan Basement bare of Upper Jurassic reservoir rocks (cf. Landshut-Neuoetting Rise)

Northern limit of the Subalpine (aka Folded, aka Imbricated) Molasse overthrusting the southern Molasse Basin deposits (cf. Hotlime Unit Subalpine Molasse)

Formation permeability distribution pattern of the Upper Jurassic carbonates underneath the Central Molasse Basin (modified after Birner et al. 2012, cf. Factsheet Permeability) to be considered in the context with inferred isolines and Helvetic Basin facies.

Inferred formation permeability distribution pattern of the Upper Jurassic carbonates underneath the Central Molasse Basin (modified after Birner et al. 2012, cf. Factsheet Permeability) to be considered in the context with 'isolines of permeability' and Helvetic Basin facies.

Transition zone to low permeability facies (less than 1 E-7) of the Helvetic Basin underneath Subalpine Molasse and Alpine nappes (cf. HotLime Unit Helvetic Facies of Upper Jurassic); to be considered in the context of formation permeability distribution isolines.

Heat in Place, the maximum theoretically extractable heat energy in the reservoir, calculated for a re-injection temperature of 18�C, expressed in GJ/m2 related to 500m x 500m x reservoir gross-thickness [m] volume units(cf. Factsheet Heat-in-Place)

Heat in Place, the maximum theoretically extractable heat energy in the reservoir, calculated for a re-injection temperature of 50�C, expressed in GJ/m2 related to 500m x 500m x reservoir gross-thickness [m] volume units (cf. Factsheet Heat-in-Place)

The gross thickness of the carbonate geothermal reservoir is one of the crucial parameters for the volumetric Heat-in-Place assessment as applied in HotLime, (cf. Factsheet Heat-in-Place).

Upper Jurassic carbonates in the Molasse Basin-Carpathian Foredeep transition zone (AT/CZ)

Click the line and follow the link to retrieve the cross-section with the reservoir rock suite color-coded in accord with International Chronostratigraphic Chart.

Heat in Place, the maximum theoretically extractable heat energy in the reservoir, calculated for a re-injection temperature of 18�C, expressed in GJ/m2 related to 500m x 500m x reservoir gross-thickness [m] volume units.

Heat in Place, the maximum theoretically extractable heat energy in the reservoir, calculated for a re-injection temperature of 50�C, expressed in GJ/m2 related to 500m x 500m x reservoir gross-thickness [m] volume units.

The gross thickness of the carbonate geothermal reservoir is one of the crucial parameters for the volumetric Heat-in-Place assessment as applied in HotLime, (cf. Factsheet Heat-in-Place).

Carboniferous carbonates in Lough Allen Basin (IE)

Click the line and follow the link to retrieve the cross-section with the reservoir rock suite color-coded in accord with International Chronostratigraphic Chart.

Fault traces at the surface as the most reliable targets in geothermal prospectivity screening. Major faults and fault zones are primary conduits for hydrothermal fluids and zones of possibly higher, but not quantifiable Heat-in-Place (cf. Factsheet Faults, Factsheet Heat-in-Place)

Heat in Place, the maximum theoretically extractable heat energy in the reservoir, calculated for a re-injection temperature of 18�C, expressed in GJ/m2 related to 500m x 500m x reservoir gross-thickness [m] volume units.

The gross thickness of the carbonate geothermal reservoir is one of the crucial parameters for the volumetric Heat-in-Place assessment as applied in HotLime, (cf. Factsheet Heat-in-Place).

Carboniferous carbonates in Dublin Basin (IE)

Click the line and follow the link to retrieve the cross-section with the reservoir rock suite color-coded in accord with International Chronostratigraphic Chart.

Heat in Place, the maximum theoretically extractable heat energy in the reservoir, calculated for a re-injection temperature of 18�C, expressed in GJ/m2 related to 500m x 500m x reservoir gross-thickness [m] volume units.

The gross thickness of the carbonate geothermal reservoir is one of the crucial parameters for the volumetric Heat-in-Place assessment as applied in HotLime, (cf. Factsheet Heat-in-Place).

Dinantian carbonates at the flanks of the London-Brabant Massif (NL/BE)

Click the line and follow the link to retrieve the cross-section with the reservoir rock suite color-coded in accord with International Chronostratigraphic Chart.

Heat in Place, the maximum theoretically extractable heat energy in the reservoir, calculated for a re-injection temperature of 18�C, expressed in GJ/m2 related to 500m x 500m x reservoir gross-thickness [m] volume units.

Heat in Place, the maximum theoretically extractable heat energy in the reservoir, calculated for a re-injection temperature of 50�C, expressed in GJ/m2 related to 500m x 500m x reservoir gross-thickness [m] volume units.

The gross thickness of the carbonate geothermal reservoir is one of the crucial parameters for the volumetric Heat-in-Place assessment as applied in HotLime, (cf. Factsheet Heat-in-Place).

Upper Triassic to Middle Eocene carbonates of the Po Basin (IT)

Click the line and follow the link to retrieve the cross-section with the reservoir rock suite color-coded in accord with International Chronostratigraphic Chart.

Heat in Place, the maximum theoretically extractable heat energy in the reservoir, calculated for a re-injection temperature of 18�C, expressed in GJ/m2 related to 500m x 500m x reservoir gross-thickness [m] volume units.

Heat in Place, the maximum theoretically extractable heat energy in the reservoir, calculated for a re-injection temperature of 50�C, expressed in GJ/m2 related to 500m x 500m x reservoir gross-thickness [m] volume units.

The gross thickness of the carbonate geothermal reservoir is one of the crucial parameters for the volumetric Heat-in-Place assessment as applied in HotLime, (cf. Factsheet Heat-in-Place).

Triassic carbonates of the Krsko-Brezice sub-basin (SI)

Click the line and follow the link to retrieve the cross-section with the reservoir rock suite color-coded in accord with International Chronostratigraphic Chart.

Heat in Place, the maximum theoretically extractable heat energy in the reservoir, calculated for a re-injection temperature of 18�C, expressed in GJ/m2 related to 500m x 500m x reservoir gross-thickness [m] volume units.

Heat in Place, the maximum theoretically extractable heat energy in the reservoir, calculated for a re-injection temperature of 50�C, expressed in GJ/m2 related to 500m x 500m x reservoir gross-thickness [m] volume units.

The gross thickness of the carbonate geothermal reservoir is one of the crucial parameters for the volumetric Heat-in-Place assessment as applied in HotLime, (cf. Factsheet Heat-in-Place).

Miocene and Triassic carbonates of Zagreb hydrothermal field (HR)

Click the line and follow the link to retrieve the cross-section with the reservoir rock suite color-coded in accord with International Chronostratigraphic Chart.

Heat in Place, the maximum theoretically extractable heat energy in the reservoir, calculated for a re-injection temperature of 18�C, expressed in GJ/m2 related to 500m x 500m x reservoir gross-thickness [m] volume units.

Heat in Place, the maximum theoretically extractable heat energy in the reservoir, calculated for a re-injection temperature of 50�C, expressed in GJ/m2 related to 500m x 500m x reservoir gross-thickness [m] volume units.

The gross thickness of the carbonate geothermal reservoir is one of the crucial parameters for the volumetric Heat-in-Place assessment as applied in HotLime, (cf. Factsheet Heat-in-Place).

Triassic carbonates of the Pantelleria-Linosa-Malta rift complex (MT)

Click the line and follow the link to retrieve the cross-section with the reservoir rock suite color-coded in accord with International Chronostratigraphic Chart.

Heat in Place, the maximum theoretically extractable heat energy in the reservoir, calculated for a re-injection temperature of 18�C, expressed in GJ/m2 related to 500m x 500m x reservoir gross-thickness [m] volume units.

Heat in Place, the maximum theoretically extractable heat energy in the reservoir, calculated for a re-injection temperature of 50�C, expressed in GJ/m2 related to 500m x 500m x reservoir gross-thickness [m] volume units.

Eocene carbonates of the Empord� Basin (ES)

Click the line and follow the link to retrieve the cross-section with the reservoir rock suite color-coded in accord with International Chronostratigraphic Chart.

Heat in Place, the maximum theoretically extractable heat energy in the reservoir, calculated for a re-injection temperature of 18�C, expressed in GJ/m2 related to 500m x 500m x reservoir gross-thickness [m] volume units.

Heat in Place, the maximum theoretically extractable heat energy in the reservoir, calculated for a re-injection temperature of 50�C, expressed in GJ/m2 related to 500m x 500m x reservoir gross-thickness [m] volume units.

The gross thickness of the carbonate geothermal reservoir is one of the crucial parameters for the volumetric Heat-in-Place assessment as applied in HotLime, (cf. Factsheet Heat-in-Place).

Triassic carbonates of Tuscan, Umbria and Marche nappes in the Umbria Trough (IT)

Click the line and follow the link to retrieve the cross-section with the reservoir rock suite color-coded in accord with International Chronostratigraphic Chart.

Heat in Place, the maximum theoretically extractable heat energy in the reservoir, calculated for a re-injection temperature of 18�C, expressed in GJ/m2 related to 500m x 500m x reservoir gross-thickness [m] volume units.

Heat in Place, the maximum theoretically extractable heat energy in the reservoir, calculated for a re-injection temperature of 50�C, expressed in GJ/m2 related to 500m x 500m x reservoir gross-thickness [m] volume units.

The gross thickness of the carbonate geothermal reservoir is one of the crucial parameters for the volumetric Heat-in-Place assessment as applied in HotLime, (cf. Factsheet Heat-in-Place).