Blar i forfatter "Sliwinska, Kasia"

Viser treff 1-3 av 3

    • The Lower Cretaceous of Svalbard and its relevance for exploration in the northern Barents Sea 

      Grundvåg, Sten-Andreas; Jelby, Mads; Midtkandal, Ivar; Sliwinska, Kasia; Nøhr-Hansen, Henrik; Marin Restrepo, Dora Luz; Kairanov, Bereke; Escalona, Alejandro; Olaussen, Snorre (Conference object; Konferansebidrag, 2017)
      The Lower Cretaceous succession in the Barents Sea is listed as a potential play model by the Norwegian Petroleum Directorate. Reservoirs may occur in deep to shallow marine clastic wedges located in proximity to palaeo-highs and along basin margins. In addition, shelf-prism-scale clinoforms with high amplitude anomalies in their top- and bottomsets have been reported from reflection seismic but ...

    • The Lower Cretaceous succession of the northwestern Barents Shelf: Onshore and offshore correlations 

      Grundvåg, Sten-Andreas; Marin Restrepo, Dora Luz; Kairanov, Bereke; Sliwinska, Kasia; Nøhr-Hansen, Henrik; Jelbye, Mads; Escalona Varela, Alejandro; Olaussen, Snorre (Journal article; Tidsskriftartikkel; Peer reviewed, 2017-06-24)
      The Lower Cretaceous succession in the Barents Sea is listed as a potential play model by the Norwegian Petroleum Directorate. Reservoirs may occur in deep to shallow marine clastic wedges located in proximity to palaeo-highs and along basin margins. In addition, shelf-prism-scale clinoforms with high amplitude anomalies in their top- and bottomsets have been reported from reflection seismic but ...

    • The role of shelf morphology on storm-bed variability and stratigraphic architecture, Lower Cretaceous, Svalbard 

      Grundvåg, Sten-Andreas; Jelby, Mads Engholm; Olaussen, Snorre; Sliwinska, Kasia (Journal article; Tidsskriftartikkel; Peer reviewed, 2020-08-13)
      The dominance of isotropic hummocky cross‐stratification, recording deposition solely by oscillatory flows, in many ancient storm‐dominated shoreface–shelf successions is enigmatic. Based on conventional sedimentological investigations, this study shows that storm deposits in three different and stratigraphically separated siliciclastic sediment wedges within the Lower Cretaceous succession in ...