Supradetachment to rift basin transition recorded in continental to marine deposition; Paleogene Bandar Jissah Basin, NE Oman

Autor: Serck, Christopher Sæbø, Braathen, Alvar, Olaussen, Snorre, Osmundsen, Per Terje, Midtkandal, Ivar, van Yperen, Anna Elisabeth, Indrevær, Kjetil

Publikováno v: Serck, Christopher Sæbø Braathen, Alvar Olaussen, Snorre Osmundsen, Per Terje Midtkandal, Ivar van Yperen, Anna Elisabeth Indrevær, Kjetil . Supradetachment to rift basin transition recorded in continental to marine deposition; Paleogene Bandar Jissah Basin, NE Oman. Basin Research. 2020
Basin Research

Externí odkaz: http://hdl.handle.net/10852/78371
https://www.duo.uio.no/bitstream/handle/10852/78371/4/bre.12484.pdf

Late Devonian–Carboniferous faulting and controlling structures and fabrics in NW Finnmark

Autor: Koehl, Jean-Baptiste P., Bergh, Steffen G, Osmundsen, Per Terje, Redfield, Thomas Fitzmaurice, Indrevær, Kjetil, Lea, Halldis, Bergø, Espen

Publikováno v: Koehl J-B, Bergh SG, Osmundsen PT, Redfield TF, Indrevær K, Lea H, Bergø E. Late Devonian–Carboniferous faulting and controllingstructures and fabrics in NW Finnmark. Norwegian Jo

Externí odkaz: https://hdl.handle.net/10037/18392

Linking onshore-offshore basement rock architecture and brittle faults on the submerged strandflat along the SW Barents Sea margin, using high-resolution (5 x 5 m) bathymetry data.

Autor: Indrevær, Kjetil^1,2 kjetil.indrevar@uit.no, Bergh, Steffen G.¹

Publikováno v: Norwegian Journal of Geology / Norsk Geologisk Forening. 2014, Vol. 94 Issue 1, p1-34. 34p.

Crustal scale subsidence and uplift caused by metamorphic phase changes in the lower crust: A model for the evolution of the Loppa High area, SW Barents Sea, from late Paleozoic to Present.

Autor: Indrevær, Kjetil, Gac, Sebastien, Gabrielsen, Roy Helge, Faleide, Jan Inge

Publikováno v: Indrevær, Kjetil Gac, Sebastien Gabrielsen, Roy Helge Faleide, Jan Inge . Crustal scale subsidence and uplift caused by metamorphic phase changes in the lower crust: A model for the evolution of the Loppa High area, SW Barents Sea, from late Paleozoic to Present.. Jo
Jo

Externí odkaz: http://hdl.handle.net/10852/59423
https://www.duo.uio.no/bitstream/handle/10852/59423/1/Indrev%25C3%25A6r_etal_2017_Revised.pdf

Post-Caledonian brittle fault zones on the hyperextended SW Barents Sea margin: New insights into onshore and offshore margin architecture.

Autor: Indrevær, Kjetil^1,2 kjetil.indrevar@uit.no, Bergh, Steffen G.¹, Koehl, Jean-Baptiste¹, Hansen, John-Are¹, Schermer, Elizabeth R.³, Ingebrigtsen, Arild²

Publikováno v: Norwegian Journal of Geology / Norsk Geologisk Forening. 2013, Vol. 93 Issue 3/4, p167-188. 22p.