| nhku-2 |
Cromer Knoll Group with Lysing Formation and younger sandstones |
Cenomanian - Campanian |
Halten Terrace, Dønna Terrace, Rås Basin |
Sandstone |
Shallow marine to deep marine |
Mainly stratigraphic |
Upper Jurassic shale (Spekk Formation) and possibly Cretaceous shale |
Identification and mapping of reservoir, reservoir thickness and quality, trap definition |
|
|
|
| nhku-3 (unconfirmed) |
Cromer Knoll Group with the Lysing Formation, Shetland Group with Kvitnos, Nise and Springar Formations |
Turon - Maastrichtian |
Ribban Basin, Lofoten Basin, Utrøst High |
Sandstone |
Shallow marine to deep marine |
Mainly stratigraphic |
Upper Jurassic shale (Spekk Formation) and possibly Cretaceous shale |
Identification and mapping of reservoir, reservoir thickness and quality, trap definition |
|
|
|
| nhku-4 |
Cromer Knoll Group with the Lysing Formation, Shetland Group with Kvitnos, Nise and Springar Formations, possibly sands of Paleocene age (Rogaland Group) |
Late Cretaceous (undifferentiated) to Early Paleocene |
Nyk High, Fenris Graben, Gjallar Ridge, Vigrid Syncline, Møre Basin (western part) |
Sandstone |
Shallow marine to deep marine |
Mainly stratigraphic |
Upper Jurassic shale (Spekk Formation) and possibly Cretaceous shale |
Identification and mapping of reservoir, reservoir thickness and quality, trap definition |
|
|
|
| nhku-5 (unconfirmed) |
Upper Cretaceous undifferentiated |
Late Cretaceous (undifferentiated) |
Træna Basin, Utgard High, Vestfjorden Basin |
Sandstone |
Shallow marine to deep marine |
Mainly stratigraphic |
Upper Jurassic shale (Spekk Formation) and possibly Cretaceous shale |
Identification and mapping of reservoir, reservoir thickness and quality, trap definition |
|
|
|
| nhku-6 |
Cromer Knoll-Group |
Cenomanian - Coniacian |
Slørebotn Sub-basin |
Sandstone |
Shallow marine to deep marine |
Mainly stratigraphic |
Upper Jurassic shale (Spekk Formation) and possibly Cretaceous shale |
Identification and mapping of reservoir, reservoir thickness and quality, trap definition |
|
|
|