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Effect of diagenesis on pore pressures in fine-grained rocks in the Egersund Basin, Central North Sea 
Kalani, Mohsen; Zadeh, Mohammad Koochak; Jahren, Jens; Mondol, Nazmul Haque; Faleide, Jan Inge (Journal article / Tidsskriftartikkel / PublishedVersion; Peer reviewed, 2015)
Pore pressure in fine-grained rocks is important with respect to drilling problems such as kicks, blowouts, borehole instability, stuck pipe and lost circulation. In this study, a succession of overpressured, fine-grained, ...
The T-Reflection and the Deep Crustal Structure of the Vøring Margin, Offshore mid-Norway 
Abdelmalak, Mohamed Mansour; Faleide, Jan Inge; Planke, Sverre; Gernigon, Laurent; Zastrozhnov, Dmitry; Shephard, Grace; Myklebust, Reidun (Journal article / Tidsskriftartikkel / PublishedVersion; Peer reviewed, 2017)
Seismic reflection data along volcanic passive margins frequently provide imaging of strong and laterally continuous reflections in the middle and lower crust. We have completed a detailed 2‐D seismic interpretation of the ...
Jurassic to Early Cretaceous basin configuration(s) in the Fingerdjupet Subbasin, SW Barents Sea 
Serck, Christopher Sæbø; Faleide, Jan Inge; Braathen, Alvar; Kjølhamar, Bent; Escalona Varela, Alejandro (Journal article / Tidsskriftartikkel / AcceptedVersion; Peer reviewed, 2017)
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 ...
The tectonized central peak of the Mjølnir Impact Crater, Barents Sea 
Corseri, Romain; Gac, Sebastien; Faleide, Jan Inge; Planke, Sverre (Journal article / Tidsskriftartikkel / AcceptedVersion; Peer reviewed, 2020)
The Mjølnir structure, SW Barents Sea, is one of the best-preserved marine impact craters on Earth. After impact on the paleo-seafloor about 142 Ma ago, this crater experienced an atypical deformation of its central peak, ...
A new tectono-magmatic model for the Lofoten/Vesterålen Margin at the outer limit of the Iceland Plume influence 
Breivik, Asbjørn Johan; Faleide, Jan Inge; Mjelde, Rolf; Flueh, Ernst R.; Murai, Yoshio (Journal article / Tidsskriftartikkel / AcceptedVersion; Peer reviewed, 2017)
The Early Eocene continental breakup was magma-rich and formed part of the North Atlantic Igneous Province. Extrusive and intrusive magmatism was abundant on the continental side, and a thick oceanic crust was produced up ...
Tectonic implications of the lithospheric structure across the Barents and Kara shelves 
Faleide, Jan Inge; Pease, Victoria; Curtis, Mike; Klitzke, Peter; Minakov, Alexander; Scheck-Wenderoth, Magdalena; Kostyuchenko, Sergei; Zayonchek, Andrei (Journal article / Tidsskriftartikkel / SubmittedVersion, 2017)
This paper considers the lithospheric structure and evolution of the wider Barents–Kara Sea region based on the compilation and integration of geophysical and geological data. Regional transects are constructed at both ...
Middle to Late Devonian–Carboniferous collapse basins on the Finnmark Platform and in the southwesternmost Nordkapp basin, SW Barents Sea 
Koehl, Jean-Baptiste; Bergh, Steffen G; Henningsen, Tormod; Faleide, Jan Inge (Journal article / Tidsskriftartikkel / PublishedVersion; Peer reviewed, 2018)
The SW Barents Sea margin experienced a pulse of extensional deformation in the Middle–Late Devonian through the Carboniferous, after the Caledonian Orogeny terminated. These events marked the initial stages of formation ...
Dyke emplacement and crustal structure within a continental large igneous province, northern Barents Sea 
Minakov, Alexander; Yarushina, Viktoriya M.; Faleide, Jan Inge; Krupnova, Natalia; Sakoulina, Tamara; Dergunov, Nikolay; Glebovsky, Vladimir (Journal article / Tidsskriftartikkel / AcceptedVersion; Peer reviewed, 2017)
We perform an integrated analysis of magnetic anomalies, multichannel seismic and wide-angle seismic data across an Early Cretaceous continental large igneous province in the northern Barents Sea region. Our data show that ...
Regional tectono-sedimentary development of the highs and basins of the northwestern Barents Shelf 
Anell, Ingrid Margareta; Faleide, Jan Inge; Braathen, Alvar (Journal article / Tidsskriftartikkel / PublishedVersion; Peer reviewed, 2016)
While many structural elements on the northwestern Barents Shelf initiated early and have remained influential on accommodation and sedimentation, detailed seismic interpretation attests to the development of new structural ...
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. 
Indrevær, Kjetil; Gac, Sebastien; Gabrielsen, Roy Helge; Faleide, Jan Inge (Journal article / Tidsskriftartikkel / AcceptedVersion; Peer reviewed, 2017)
The Loppa High area has been subject to several events of uplift and subsidence from the Late Paleozoic to Present. The driving mechanisms behind the vertical movements, however, are not fully understood. We propose that ...
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