EGDI (v1.6.16027)

« GARAH

Base layers

Layers

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)

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Details

« GARAH

Geological Analysis and Resource Assessment of selected Hydrocarbon systems

Layers

Geology