Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Christopher Sæbø Serck"'
Autor:
Jan Inge Faleide, Christopher Sæbø Serck, Per Terje Osmundsen, Julie Linnéa Sehested Gresseth, Alvar Braathen
Publikováno v:
Basin Research
Late to post-Caledonian, Devonian extension remains unresolved in the SW Barents Sea, despite considerable knowledge from onshore Norway, East Greenland and Svalbard. We analyse intrabasement seismic facies in high-resolution 3D and reprocessed 2D da
Autor:
Thea Sveva Faleide, Romain Corseri, Christopher Sæbø Serck, Ivar Midtkandal, Johan Petter Nystuen, Myrsini Dimitriou, Sverre Planke, Jan Inge Faleide
Publikováno v:
Geological Magazine. 157:458-476
A comprehensive dataset is collated in a study on sediment transport, timing and basin physiography during the Early Cretaceous Period in the Boreal Basin (Barents Sea), one of the world’s largest and longest active epicontinental basins. Long-wave
Publikováno v:
Geological Society, London, Special Publications. 495:29-41
While the Triassic is comparatively a tectonically quiescent period in the dynamic development of the Barents Shelf, the depositional infill was strongly influenced by structural elements and there is a marked difference between lower and middle Tria
Autor:
Christopher Sæbø Serck, Alvar Braathen
Publikováno v:
Basin Research. 31:967-990
Extensional faults and folds exert a fundamental control on the location, thickness and partitioning of sedimentary deposits on rift basins. The connection between the mode of extensional fault reactivation, resulting fault shape and extensional fold
Autor:
Sverre Planke, Thea Sveva Faleide, Romain Corseri, Christopher Sæbø Serck, Mikal Trulsvik, Ivar Midtkandal, Jan Inge Faleide
Publikováno v:
Marine and Petroleum Geology. 98:462-476
Mud-rich prograding sediment lobes make for most of the Barremian – Albian stratigraphic record in the SW Barents Sea. Submarine canyons and channels potentially represent key components of sediment transport from shelf to basin floor but geologica
Autor:
Kjetil Indrevær, Snorre Olaussen, Christopher Sæbø Serck, Per Terje Osmundsen, Anna E. van Yperen, Ivar Midtkandal, Alvar Braathen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4e9741cd4d76e7ca7a5d841ad367d5c4
https://doi.org/10.1111/bre.12484/v2/response1
https://doi.org/10.1111/bre.12484/v2/response1
Autor:
Snorre Olaussen, Christopher Sæbø Serck, Alvar Braathen, Anna E. van Yperen, Per Terje Osmundsen, Ivar Midtkandal, Kjetil Indrevær
Publikováno v:
Basin Research
A transition from supradetachment to rift basin signature is recorded in the ~1,500 m thick succession of continental to shallow marine conglomerates, mixed carbonate‐siliciclastic shallow marine sediments and carbonate ramp deposits preserved in t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::09791028c951d6cca3c87cc0a45805a0
https://hdl.handle.net/11250/2677555
https://hdl.handle.net/11250/2677555
Autor:
Ivar Midtkandal, Thea Sveva Faleide, Christopher Sæbø Serck, Jan Inge Faleide, Johan Petter Nystuen, Romain Corseri, Sverre Planke
Regional Early Cretaceous uplift of the northern Barents Sea associated with the High Arctic Large Igneous Province (HALIP) caused the development of the fluvial to open-marine depositional system, terminating in the southwestern Barents Sea. This st
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8b448ac6453d72977400ca1f3f30eaf4
http://hdl.handle.net/10852/76190
http://hdl.handle.net/10852/76190
Publikováno v:
Marine and Petroleum Geology
The Fingerdjupet Subbasin in the southwestern Barents Sea sits in a key tectonic location between deep rifts in the west and more stable platform areas in the east. Its evolution is characterized by extensional reactivation of N-S and NNE-SSW faults
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::acb66a15336ee2870d2e1e24fa83c0f8
http://hdl.handle.net/11250/2567045
http://hdl.handle.net/11250/2567045