East Greenland and Mid-Norway
East Greenland forms part of the western margin of the North Atlantic Rift system. Its onshore geology is closely comparable to the geology of offshore Mid-Norway, the northern North Sea and the Faroe-Shetland region. Excellent exposures of Palaeozoic, Mesozoic and Cenozoic strata provide direct analogues for the adjacent offshore basins within the North Atlantic rift, which contain important hydrocarbon resources and are of increasing importance for CO2 storage in saline aquifers.
Map of Region
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Most Recent Reports
- Permian Source Rock Study II: Palynology of the Ravnefjeld Formation and overlying mudstones
- Permian Source Rock Study II: Geochemistry of the Ravnefjeld Formation and overlying mudstones
- Permian source rock study: Sedimentology of the Ravnefjeld Formation and overlying mudstones
- Permian Source Rock Study: Geochemistry of the Ravnefjeld Formation and overlying mudstones
- Mid Jurassic to Early Cretaceous review – Part 7: Traill Ø and Geographical Society Ø