EGDI (v1.6.16027)

Hydrocarbon fields

Bo member

100 m Kimmeridge Clay and equivalents

Kimmeridge Clay and equivalents

Posidonia and equivalents

Sleen Formation

Bowland and equivalents

Bo Member and equivalents

100 m Kimmeridge Clay and equivalents

Kimmeridge Clay and equivalents

Posidonia and equivalents

Sleen Formation

Shallow Gas

Eocene

Lower Eocene

Paleocene

Upper Cretaceous

Lower Cretaceous

Upper Jurassic

Middle Jurassic

Lower Jurassic

Triassic

Zechstein

Permian Rotliegend

Carboniferous

Devonian

Profile line

GIIP

OIIP

Vitrinite reflectance at the Base Cretaceous Unconformity subcrop.

Average vitrinite reflectance for the Upper Jurassic

Average transformation ratio for the Upper Jurassic

Average vitrinite reflectance for the Lower Jurassic

Vitrinite reflectance at the Top Lower Jurassic

Average transformation ratio for the Lower Jurassic

Wells used for calibration

Study area

Profile line

Source rocks

Modelled accumulation of hydrocarbons

Study area

Salt Structures

Basins and highs (from NAG-TEC)

Ages of structural elements (from NAG-TEC)

Regions of structural elements (from NAG-TEC)

CO2 Storage

Area of interest

Susceptibility

Susceptibility Reliability

Knowledge gap assessment of hydrate evidence and indicators

Knowledge gap analysis of geothermal gradient data.

Knowledge gap analysis of seafloor temperature data

Evidence and indicators for gas hydrates. Point data.

Evidence and indicators for gas hydrates. Polygons.

Gas analyses from IODP Drilling holes

Geophysical indicators. Point data

Geophysical indicators for gas hydrates. Lines.

Geophysical indicators for gas hydrates. Polygons

Seafloor features that indicate fluid flow. Point data.

Seafloor features that indicate fluid flow. Polygons.

Base of negative bouyancy zone for 96% C02. South of Biscay Bay, Galicia Area

Base of negative bouyancy zone for 96% C02. Extended 200M in the FISU Area, Celtic Sea.

Base of negative bouyancy zone for 96% C02. Celtic Sea & French EEZ

Base of negative bouyancy zone for 100% C02. Celtic Sea & French EEZ

Base of hydrate stability zone for 96% CO2. South of Biscay Bay, Galicia Area.

Base of hydrate stability zone for 96% CO2. Extended 200M in the FISU Area, Celtic Sea.

Base of hydrate stability zone for 96% CO2. Celtic Sea & French EEZ

Base of hydrate stability zone for 100% CO2. Celtic Sea & French EEZ.

Base of hydrate stability zone for biogenic gas. NW Europe

Base of hydrate stability zone for biogenic gas. SW Europe.

Base of hydrate stability zone for biogenic gas. From Pi�ero et al. 2013.

Seafloor temperatures

Heat flow

Bathymetry

Europa offshore faults (IGME 5000)

Sediment accumulation rate cm/year

Sediment thickness, m

Wells (from EMODnet)

Active licences (from EMODnet))

Pipelines

Infrastructure (point data)

Average Surface Swept Area Ratio 2015-2018

Windfarms from EMODnet (polygons)

Windfarms from EMODnet (points)

EEZ (lines)

Areas of Interest

Units (overview) - Structural Framework of Bavaria

Limit uncertainty (overview) - Structural Framework of Bavaria

Limits (overview) - Structural Framework of Bavaria

Units (detail) - Structural Framework of Bavaria

Limit uncertainty (detail) - Structural Framework of Bavaria

Limits (detail) - Structural Framework of Bavaria

Units (overview) - Structural Framework of Ireland

Limit uncertainty (overview) - Structural Framework of Ireland

Limits (overview) - Structural Framework of Ireland

Units (detail) - Structural Framework of Ireland

Limit uncertainty (detail) - Structural Framework of Ireland

Limits (detail) - Structural Framework of Ireland

Geomanifestations - Ireland

Units (overview) - Structural Framework of the Pannonian Basin

Limit uncertainty (overview) - Structural Framework of the Pannonian Basin

Limits (overview) - Structural Framework of the Pannonian Basin

Units (detail) - Structural Framework of the Pannonian Basin

Limit uncertainty (detail) - Structural Framework of the Pannonian Basin

Limits (detail) - Structural Framework of the Pannonian Basin

Geomanifestations - Pannonian Basin

Units (overview) - Structural Framework of R2R

Limit uncertainty (overview) - Structural Framework of R2R

Limits (overview) - Structural Framework of R2R

Units (detail) - Structural Framework of R2R

Limit uncertainty (detail) - Structural Framework of R2R

Limits (detail) - Structural Framework of R2R

Geomanifestations (part 1) - R2R

Geomanifestations (part 2) - R2R

Geomanifestations (part 3) - R2R

Current plates

Paleoplates

Lithotectonic units

Orogens

Deformation zones

Basins

Limit Uncertainty - Pan-Eu Structural Framework

Limits - Pan-Eu Structural Framework

Fault Database Details

Fault Database Overview

Fault Database Polygons

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)

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

Ljubljana pilot area

Link�ping pilot area

Zaragoza pilot area

Zagreb pilot area

Aarhus pilot area

Girona pilot area

Prague pilot area

Vienna pilot area

Cardiff pilot area

Glasgow pilot area

Specific yield, Zaragoza

Extent of confined artesian and subartesian aquifers, Bratislava

Extent of confined artesian and subartesian aquifers, Warsaw

Extent of confined artesian and subartesian aquifers, Brussels

Compressible ground, Cork

Net aquifer thickness, Cardiff

Net aquifer thickness, Aarhus

Net aquifer thickness, Zaragoza

Specific annual thermal load CLS, Vienna

Net thickness of the shallow karst aquifer, Cork

Net thickness of the deep karst aquifer, Cork

Net thickness of sand and gravel aquifers, Cork

Hydraulic conductivity of an alluvial aquifer, Zaragoza

Land surface temperature, Vienna

Land surface temperature, Zagreb

Land surface temperature, Girona

Land surface temperature, Bratislava

Groundwater protection, Link�ping

Land surface temperature, Ljubljana

Land surface temperature, Brussels

Land surface temperature, Cork

Land surface temperature, Prague

Mining areas, Warsaw

Mining areas, Prague

Other groundwater use, Aarhus

Other groundwater use, Warsaw

Other groundwater use, Link�ping

Other groundwater use, Zaragoza

Groundwater body suitable for open-loop systems, Bratislava

Other groundwater use, Brussels

Other groundwater use, Cork

Other groundwater use, Prague

Shallow geothermal energy systems, Link�ping

Shallow geothermal energy systems, Brussels

Groundwater protection, Zagreb

Groundwater protection, Bratislava

Groundwater protection, Link�ping

Faults, Prague

Groundwater protection, Brussels

Hydraulic transmissivity of the Quaternary aquifer, Girona

Hydraulic transmissivity of the Neogene aquifer, Girona

Hydraulic transmissivity of the Eocene aquifer, Girona

Hydraulic transmissivity of the karst shallow aquifer, Cork

Hydraulic transmissivity of the karst deep aquifer, Cork

Hydraulic transmissivity of gravel aquifer, Cork

Landslides, Warsaw

Landslides, Cork

Landslides, Prague

Bratislava pilot area

Groundwater protection, Prague

Groundwater protection, Warsaw

Groundwater protection, Vienna

Groundwater protection, Aarhus

Groundwater protection, Ljubljana

Shallow geothermal energy systems, Prague

Shallow geothermal energy systems, Cardiff

Shallow geothermal energy systems, Cork

Shallow geothermal energy systems, Zaragoza

Shallow geothermal energy systems, Warsaw

Shallow geothermal energy systems, Aarhus

Faults, Link�ping

Faults, Cork

Groundwater disposal, Zaragoza

Cork pilot area

Brussels pilot area

Warsaw pilot area

Hydraulic conductivity of karst aquifers, Cork

Hydraulic conductivity of gravel aquifers, Cork

Net thickness of the Eocene aquifer, Girona

Net thickness of the shallow Neogene, Girona

Net thickness of the Quaternary aquifer, Girona

Measured subsurface temperature profile, Bratislava

Average interval subsurface temperature, Girona

Minimum groundwater temperature, Bratislava

Potentially karstified zones, Cork

Potentially karstified zones, Prague

Natural reserves, Bratislava

Hydraulic productivity, Bratislava

In-situ thermal conductivity of unconsolidated sediments, Bratislava

Hydraulic transmissivity of the Quaternary aquifer, Girona

Subsurface infrastructure, Cork

Decision support map, Aarhus

Hydraulic conductivity, Vienna

Groundwater body suitable for open-loop systems, Cork

Groundwater body suitable for open-loop systems, Aarhus

Heat transfer rate CLS, Vienna

Geological cross-section, Cork

Specific hydraulic productivity, Vienna

Traffic light map for open loop system

Average interval subsurface temperature, Vienna

Specific yield bedrock lI aquifer, Cork

Traffic light map for closed loop system

Average interval bulk thermal conductivity, Vienna

Specific yield bedrock aquifer, Cork

Geological cross-section, Aarhus

Maximum groundwater temperature, Vienna

Specific yield gravel aquifers, Cork

Thermal productivity, Bratislava

Measured groundwater depth, Girona

Minimun groundwater temperature, Vienna

Thermal conductivity hard rock sample, Cork

Specific Thermal capacity OLS, Bratislava

Specific annual thermal load OLS, Vienna

Net aquifer thickness, Vienna

Measured Groundwater level April 2019, Cork

Groundwater body suitable for open-loop systems, Vienna

Measured Groundwater level November 2019, Cork

Natural reserves, Vienna

Contaminated sites, Cork

Average interval subsurface temperature, Ljubljana

Natural reserves, Prague

Measured groundwater depth, Cork 11/2019

Traffic light map closed loop systems, Ljubljana

Measured groundwater depth, Cork 08/2020

Critical chemical composition of groundwater, Bratislava

Annual thermal load, Girona

Natural reserves, Warsaw

Flood hazards, Cork

Specific thermal capacity, Ljubljana

Measured subsurface temperature profile, Cardiff

Specific annual thermal load, Ljubljana

Contaminated sites, Bratislava

Geological cross-section, Cardiff

Minimum groundwater temperature, Ljubljana

Average interval subsurface temperature, Cardiff

Depth of bedrock, Cardiff

Hydraulic productivity, Ljubljana

Depth of a shallow glacial gravel aquifer, Cardiff

Subsurface infrastructure, Warsaw

Measured groundwater level 2021, Bratislava

Average interval bulk thermal conductivity, Link�ping

Natural reserves, Zagreb

Measured groundwater level 2018, Bratislava

Contaminated sites, Zagreb

Specific annual thermal load OLS, Bratislava

Subsurface infrastructure, Ljubljana

Groundwater body suitable for open-loop systems, Zaragoza

Average interval subsurface temperature, Bratislava

Groundwater body suitable for open-loop systems, Ljubljana

Depth bedrock, Link�ping

Groundwater body suitable for open-loop systems, Brussels

Average interval bulk thermal conductivity, Ljubljana

Natural reserves, Brussels

Natural reserves, Ljubljana

Average interval bulk thermal conductivity, Brussels

Contaminated sites, Brussels

Thermal capacity - open loop systems, Girona

Groundwater body suitable for open-loop systems, Cardiff

Fluorine - HGT greater than 1 (1,5 mg/l)

Arsenic - HGT greater than 0,5 (5 �g/l)

Arsenic - HGT greater than 1 (10 �g/l)

Thermal Waters

Mineral Waters (national law recognition)

Natural Mineral Waters (according to Directive 2009/54/EC)

Model estimates of nitrate-N stored in the unsaturated zone

Gridded estimates of travel times for nitrate in the unsaturated zone in six european countries

Chart - Denitrification data by countries

Label - Denitrification data by countries

Pilot Studies

Tracer Data

Vulnerability Map

Depth to Watertable (10km grid resolution)

Groundwater Recharge

Aquifer Media

Soil Media

Topograhpy

Impact of Vadose Zone Media

Hydraulic Conductivity

Vulnerability Map