This study deals with the recunstruction of depositional environments and development of transgressive-regressive sequences within the upper Grumantbyen Formation and lower Frysjaodden Formation in the Central Basin. Data ...

Geologically, the Barents Sea with deep sedimentary basins, highs and platforms is a complex mosaic and formed as a result of different geologic and tectonic processes with complex geological history. The history of the ...

Den tektomagmatiske aktiviteten i Oslofeltet startet i slutten av karbon og endte muligens så sent som i trias. Tidspunktet for da den tektomagmatiske aktiviteten startet, er godt begrenset, både ved biostratigrafi og ved ...

Mobility of sand by fluidization, so-called sand tectonics, can drive surface movements and thereby have a significant impact on depositional environments. Deformation related to sand mobilization is a typical understudied ...

The Early to Middle Jurassic Stø Formation is the most commercially important sandstones reservoir in the Barents Sea. Stø Formation was deposited in a relatively shallow epicontinental sea in northern Pangea. One of the ...

A total of seventy reservoir core samples from nine wells of the Mid-Norway and the Barents Shelf were geochemically analyzed to compare the composition, alteration effects, maturation and organic facies. The analytical ...

The Sælabonn Formation belongs to the Bærum Group, and is recognized in the western part of the Oslo Region, from Mjøsa in the north to Skien in the south. The Sælabonn Formation is the lowermost unit in the Silurian ...

Svartodden leddet i Huk Formasjonen ved Slemmestad, Buskerud, har blitt undersøkt for å beskrive avsetningsmiljøet i området da sedimentene ble avsatt under tidsperioden Ordovicium. Svartodden leddet er rikt på endoceratide ...

In this study the taphonomy of a collection of 25 marine reptiles from the Slottsmøya member, (Agardhfjellet Formation) Svalbard was investigated. The marine reptiles which include ichthyosaurs, plesiosaurs and pliosaurs ...