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From rifting to drifting:effects on the development of deep-water hydrocarbon reservoirs in a passive margin setting,Norwegian Sea
deep-water hydrocarbon reservoirs passive margin setting Norwegian Sea
2009/12/3
The Cretaceous to Eocene deep-water hydrocarbon reservoirs in the Norwegian Sea were deposited during four main tectonic stages from continental rifting to oceanic drift: 1) Late Jurassic/Early Cretac...
Elevated erosion surfaces in central West Greenland and southern Norway:their significance in integrated studies of passive margin development
Elevated erosion surfaces southern Norway integrated studies passive margin development
2009/12/2
Elevated erosion surfaces were used as an independent data set in an integrated study of the landscape development in central West Greenland.The study resulted in a time-constrained model describing m...
Cenozoic landscape development on the passive margin of northern Scandinavia
Cenozoic landscape development passive margin northern Scandinavia
2009/12/2
The geometry of major bedrock landforms in a central part of the Northern Scandes has been examined for interpretation of landforming events and their chronology. Analysis of palaeosurfaces and palaeo...