Roy Helge Gabrielsen

Leever, K.A., Gabrielsen, R.H., Sokoutis, D. & Willingshofer, E., 2011: The effect of convergence angle on the kinematic evolution of strain partitioning in transpressional brittle wedges: insight from analog modeling and high resolution digital image analysis. Tectonics, 30, TC2013, 1-25, doi: 10.1029/2009TC002649

Leever, K.A., Gabrielsen, R.H., Faleide, J.I. & Braathen, A., 2011: A transpressional origin for the West Spitsbergen Fold and Thrust Belt - insight from analog modeling. Tectonics, 30, TC2014, 1- 24, doi: 10.1029/2010TC002753

Gabrielsen, R.H., Faleide, J.I., Pascal, C., Braathen, A., Nystuen, J.P., Etzelmuller, B. & O’Donnell, S., 2010: Reply to Discussion of Gabrielsen et al. (2010) by Nielsen et al. (this volume): Latest Caledonian to Present tectonomorphological development of southern Norway. Marine and Petroleum Geology, 27, 1290-1295, doi:10.1016/j.marpetgeo.2010.02.003.

Gabrielsen, R.H., 2010: The structure and hydrcarbon traps of sedimentary basins. In: Bjørlykke, K.: Petroleum Geoscience: From Sedimentary Environments to Rock Physics. Springer-Verlag, Berlin Heidelberg, 299 – 327.

Faleide, J.I., Bjørlykke, K. & Gabrielsen, R.H., 2010: Geology of the Norwegian Continental Shelf. In: Bjørlykke, K.: Petroleum Geoscience: From Sedimentary Environments to Rock Physics. Springer-Verlag, Berlin Heidelberg, 467-499.

Gabrielsen, R.H., Dypvik, H. & Shuvalov, V., 2010: Structural Analysis of Deformed Central Peak Sediments. In: Dypvik, H., Tsikalas, F. & Smelror, M. (eds.): The Mjølnir Impact Event and ist Consequences. Springer-Verlag, Berlin Heidelberg, 211-228.

Pascal, C., Roberts, D. & Gabrielsen, R.H., 2010: Tectonic significance of present-day stress relief phenomena in formerly glaciated regions. Journal of the Geological Society, London, 167, 363-371.

Gabrielsen, R.H., Faleide, J.I., Pascal, C., Braathen, A., Nystuen, J.P., Etzelmuller, B. & O’Donnell, S., 2010: Latest Caledonian to Present tectonomorphological development of southern Norway. Marine and Petroleum Geology, 27, 709-723, doi: 10.1016/j.marpetgeo.2009.06.004.

Herrevold, T., Gabrielsen, R.H. & Roberts, D., 2009: Structural geology of the southeastern part of the Trollfjorden-Komagelva Fault Zone, Varanger Peninsula, Finnmark, North Norway. Norwegian Journal of Geology, 89, 305-325.

Bastesen, E., Braathen, A., Nøttveit, H., Gabrielsen, R.H. & Skar, T., 2009: Extensional fault cores in micritic carbonate – Case studies from the Gulf of Corinth, Greece. Journal of Structural Geology, 31, 403-420.

Lindanger, M., Gabrielsen, R.H. & Braathen, A., 2007: Analysis of rock lenses in extensional faults. Norwegian Journal of Geology, 87(4), 361-372.

Pascal, C., Roberts, D. & Gabrielsen, R.H., 2005: Quantification of neotectonic stress orientations and magnitudes from field observations i Finnmark, northern Norway. Journal of Structural Geology, 27, 859-870.

Redfield, T.R., Braathen, A., Gabrielsen, R.H., Osmundsen, P.T., Torsvik, T.H. & Andriessen, P.A.M., 2005: Late Mesozoic to Early Cretaceous components of vertical separation across the Møre-Trøndelag Fault Complex, Norway. Tectonophysics, 395, 233-249.

Ehrlich, R. & Gabrielsen, R.H., 2004: The complexity of a ramp-flat-ramp fault and its effect on hanging-wall structuring: An example from the Njord oil field, offshore mid Norway. Petroleum Geoscience, 10(4), 305-317.

Lothe, A.E., Borge, H. & Gabrielsen, R.H., 2004: Modelling of hydraulic leakage by pressure and stress simulations and implications for Biot’s constant: an example from the Halten Terrace, offshore Mid-Norway. Petroleum Geoscience, 10(3), 199-213.

Redfield, T.R., Torsvik, T.H., Andriessen, P.A.M. & Gabrielsen, R.H., 2004: Mesozoic and Cenozoic tectonics of the Møre-Trøndelag Fault Complex, central Norway: constraints from new apatite fission track data. Physics and Chemistry of the Earth, 10 (29), 673-682.

Braathen, A., Osmundsen, P.T. & Gabrielsen, R.H., 2004: Dynamic development of fault rocks in a crustal-scale detachment: An example from western Norway. Tectonics, 21. TC4010, 1-21.

Lindanger, R., Øygaren, M., Gabrielsen, R.H., Mjelde, R., Randen, T. & Tjøstheim, B.A., 2004: Analogue (plaster) modelling and synthetic seismic representation hangingwall falt blocks above of ramp-flat ramp faults. First Break, 22, January 2004, 22-30.

Kyrkjebø,R., Gabrielsen, R.H. & Faleide, J.I., 2004: Unconformities related to the Jurassic-Cretaceous syn/post-rift transition of the northern North Sea. Journal of the Geological Society of London, 161, 1-17.

Faleide, J.I., Kyrkjebø, R., Kjennerud, T., Gabrielsen, R.H., Jordt, H., Fanavoll, S. & Bjerke, M.D., 2002: Tectonic impact on sedimentary processes during Cenozoic evolution of the northern North Sea and surrounding areas. In: Doré, A.G., Cartwright, J.A., Stoker, M.S., Turner,  J.P. & White, N. (eds.): Exhumation of the North Atlantic Margin: Mechanisms and Implications for Petroleum Exploration., Geological Society of London Special Publication, 196, 235-269.

Lothe, A.E., Gabrielsen, R.H., Bjørnevoll Hagen, N. & Larsen, B.T., 2002: The texture of deformation bands: effects on porosity and permeability. Petroleum Geoscience, 8, 195-207.

Gabrielsen, R.H., Kyrkjebø, R., Faleide, J.I., Fjeldskaar, W. & Kjennerud, T., 2001: The Cretaceous post-rift basin configuration of the northern North Sea. Petroleum Geoscience, 7, 137-154.

Pascal, C. & Gabrielsen, R.H., 2001: Numerical modelling of Cenozoic stress patterns in the mid Norwegian Margin and the northern North Sea. Tectonics, 20(4), 585-599.

Gabrielsen, R.H. & Clausen, J.A., 2001: Horses and duplexes in extensional regimes: A scale modeling contribution. in: H.A.Koyi & N.S.Mancktelow (eds.): Tectonic Modeling: A Volume in Honor of Hans Ramberg. Geological Society of America Memoir, 193, 219-233.

Gabrielsen, R.H., Odinsen, T. & Grunnaleite, I., 1999: Structuring of the Northern Viking Graben and the Møre Basin; the influence of basement structural grain, and the particular role of the Møre-Trøndelag Fault Complex. Marine and Petroleum Geology, 16, 443-465.

Vågnes, E., Gabrielsen, R.H. & Haremo, P., 1998: Late Cretaceous - Cenozoic intraplate contractional deformation at the Norwegian continental shelf; timing, magnitude and regional implications. Tectonophysics, 300, 29-46.

• Hassaan, Muhammad; Faleide, Jan Inge; Gabrielsen, Roy Helge & Tsikalas, Filippos (2020). Architecture of the evaporite accumulation and salt structures dynamics in Tiddlybanken Basin, southeastern Norwegian Barents Sea. Basin Research.  ISSN 0950-091X.  33(1), s 91- 117 . doi: 10.1111/bre.12456 Full text in Research Archive. Show summary

  An extensive, reprocessed two-dimensional (2D) seismic data set was utilized together with available well data to study the Tiddlybanken Basin in the southeastern Norwegian Barents Sea, which is revealed to be an excellent example of base salt rift structures, evaporite accumulations and evolution of salt structures. Late Devonian–early Carboniferous NE-SW regional extensional stress affected the study area and gave rise to three halfgrabens that are separated by a NW-SE to NNW-SSE trending horst and an affiliated interference transfer zone. The arcuate nature of the horst is believed to be the effect of pre-existing Timanian basement grain, whereas the interference zone formed due to the combined effect of a Timanian (basement) lineament and the geometrical arrangement of the opposing master faults. The interference transfer zone acted as a physical barrier, controlling the facies distribution and sedimentary thickness of three-layered evaporitic sequences (LES). During the late Triassic, the northwestern part of a salt wall was developed due to passive diapirism and its evolution was influenced by halite lithology between the three-LES. The central and southeastern parts of the salt wall did not progress beyond the pedestal stage due to lack of halite in the deepest evaporitic sequence. During the Triassic–Jurassic transition, far-field stresses from the Novaya Zemlya foldand- thrust belt reactivated the pre-salt Carboniferous rift structures. The reactivation led to the development of the Signalhorn Dome, rejuvenated the northwestern part of the salt wall and affected the sedimentation rates in the southeastern broad basin. The salt wall together with the Signalhorn Dome and the Carboniferous pre-salt structures were again reactivated during post-Early Cretaceous, in response to regional compressional stresses. During this main tectonic inversion phase, the northwestern and southeastern parts of the salt wall were rejuvenated; however, salt reactivation was minimized towards the interference transfer zone beneath the centre of the salt wall.

• Kalani, Mohsen; Faleide, Jan Inge & Gabrielsen, Roy Helge (2020). Palaeozoic-Mesozoic tectono-sedimentary evolution and magmatism of the Egersund Basin area, Norwegian central North Sea. Marine and Petroleum Geology.  ISSN 0264-8172.  122 . doi: 10.1016/j.marpetgeo.2020.104642 Full text in Research Archive.
• Gabrielsen, Roy Helge; Olesen, Odleiv; Braathen, Alvar; Faleide, Jan Inge; Baranwal, Vikas Chand & Lindholm, Conrad (2019). The Listafjorden-Drangedal fault complex of the Agder-Telemark lineament zone, southern Norway. A structural analysis based on remote sensing and potential field data. GFF.  ISSN 1103-5897.  141(3), s 200- 215 . doi: 10.1080/11035897.2019.1624978
• Gabrielsen, Roy Helge; Zalmstra, Heleen; Sokoutis, Dimitrios; Willingshofer, Ernst; Faleide, Jan Inge & Braut, Hanna Lima (2019). The influence of mechanically weak layers in controlling fault kinematics and graben configurations: Examples from analog experiments and the Norwegian continental margin. American Association of Petroleum Geologists Bulletin.  ISSN 0149-1423.  103(5), s 1097- 1110 . doi: 10.1306/10261817077 Full text in Research Archive.
• Hassaan, Muhammad; Faleide, Jan Inge; Gabrielsen, Roy Helge & Tsikalas, Filippos (2019). Carboniferous graben structures, evaporite accumulations and tectonic inversion in the southeastern Norwegian Barents Sea. Marine and Petroleum Geology.  ISSN 0264-8172.  112 . doi: 10.1016/j.marpetgeo.2019.104038 Full text in Research Archive. Show summary

  High quality reprocessed seismic reflection profiles and available wells were used to study the little studied southeastern Norwegian Barents Sea and east Finnmark Platform. The study area comprises prominent structural elements such as the Haapet, Veslekari, and Signalhorn domes, the West Fedynsky High, and the Tiddlybanken and Nordkapp basins. Seven deep-seated Carboniferous grabens, not formally described earlier, were defined and informally named; and similarly, five evaporite bodies that are tapered stratigraphically above the grabens have been mapped in detail. In the late Devonian, the region comprised a central structural high (Fedynsky High), and two depressions to the north and south, and has subsequently experienced transtensional deformation during a late Devonian-early Carboniferous NE-SW regional extensional phase. As a result, a NW-SE trending graben system was created over the paleotopography, following the inherited Timanian orogeny lineaments and giving rise to the deep-seated Carboniferous grabens. Pennsylvanian to early Permian evaporites were deposited and were characterized by mobile and non-mobile lithologies. The Carboniferous structures controlled the volume, thickness and lithological alterations of the evaporites, and have later influenced the distribution and development of the salt wall and domes. The Haapet, Veslekari, composite West Fedynsky (two domes informally named Alpha and Beta) and Signalhorn domes were generated and the salt wall of the Tiddlybanken Basin was rejuvenated during the late Triassic due to compressional stresses propagating from the evolving Novaya Zemlya fold-and-thrust belt. The domes and salt wall were subsequently reactivated during the upper Jurassic and earliest Cretaceous. Furthermore, we infer that the main phase of reactivation of these structures took place during the early-middle Eocene due to far-field stresses from the transpressional Eurekan/Spitsbergen orogeny.

• Indrevær, Kjetil; Gac, Sebastien; Gabrielsen, Roy Helge & Faleide, Jan Inge (2018). 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. Journal of the Geological Society.  ISSN 0016-7649.  175(3), s 497- 508 . doi: 10.1144/jgs2017-063 Full text in Research Archive.
• Kornprobst, Jacques; Abalos, Benito; Barbey, Pierre; Boullier, Anne-Marie; Burg, Jean-Pierre; Capdevila, Ramon; Claesson, Stefan; Cordani, Umberto; Corrigan, David; Gabrielsen, Roy Helge; Gil-Ibarguchi, Jose I.; Johansson, Åke; Letsch, Dominik; Le Vigouroux, Philippe & Upton, Brian (2018). Boris Choubert: Unrecognized visionary geologist, pioneer of the global tectonics. Bulletin de la Société Géologique de France.  ISSN 0037-9409.  189(2) . doi: 10.1051/bsgf/2018006 Full text in Research Archive.
• Lundmark, Anders Mattias; Gabrielsen, Roy Helge; Strand, Tor & Ohm, Sverre Ekrene (2018). Repeated post-Caledonian intra-cratonic rifting in the central North Sea: Evidence from the volcanic record in the Embla oil field. Marine and Petroleum Geology.  ISSN 0264-8172.  92, s 505- 518 . doi: 10.1016/j.marpetgeo.2017.11.018 Full text in Research Archive.
• Gabrielsen, Roy Helge; Braathen, Alvar; Kjemperud, Magnus Vestheim & Valdresbåten, Marie Lovise (2017). The geometry and dimensions of fault core lenses. Geological Society Special Publication.  ISSN 0305-8719.  439, s 249- 269 . doi: doi.org/10.1144/SP439.4.
• Gabrielsen, Roy Helge; Nystuen, Johan Petter & Olesen, Odleiv (2017). Fault distribution in the Precambrian basement of South Norway, Journal of Structural Geology. Journal of Structural Geology.  ISSN 0191-8141.  108, s 269- 289 . doi: 10.1016/j.jsg.2017.06.006
• Indrevær, Kjetil; Gabrielsen, Roy Helge & Faleide, Jan Inge (2017). Early Cretaceous synrift uplift and tectonic inversion in the Loppa High area, southwestern Barents Sea, Norwegian shelf. Journal of the Geological Society.  ISSN 0016-7649.  174(2), s 242- 254 . doi: 10.1144/jgs2016-066 Full text in Research Archive.
• Skar, Tore; Berg, Silje Støren; Gabrielsen, Roy Helge & Braathen, Alvar (2017). Fracture networks of normal faults in fine-grained sedimentary rocks: examples from Kilve Beach,SW England.. Geological Society Special Publication.  ISSN 0305-8719.  439, s 289- 306 . doi: 10.1144/SP439.10
• Gabrielsen, Roy Helge (2016). Natural Hazards: what are they, can the be Predicted, and can they be Prevented?, In Roy Helge Gabrielsen (ed.),  Natural disasters and societal safety.  Det Norske Videnskaps-Akademi.  ISBN 82-7719-083-2.  Introduksjon.  s 9 - 12
• Gabrielsen, Roy Helge; Braathen, Alvar; Kjemperud, Magnus Vestheim & Valdresbåten, Marie Lovise (2016). The geometry and dimensions of fault-core lenses. Geological Society Special Publication.  ISSN 0305-8719.  439 . doi: 10.1144/SP439.4
• Gabrielsen, Roy Helge; Sokoutis, Dimitrios; Willingshofer, Ernst & Faleide, Jan Inge (2016). Fault linkage across weak layers during extension: an experimental approach with reference to the Hoop Fault Complex of the SW Barents Sea. Petroleum Geoscience.  ISSN 1354-0793.  22(2), s 123- 135 . doi: 10.1144/petgeo2015-029
• Torabi, Anita; Alaei, Behzad; Kolyukhin, Dmitriy; Libak, Audun; Gabrielsen, Roy Helge & Braathen, Alvar (2016). Fault geometry and seismic attributes; an integrated study with focus on the Barents Sea. First Break.  ISSN 0263-5046.  34(5), s 51- 58
• Torabi, Anita; Gabrielsen, Roy; Fossen, Haakon; Ringrose, Philip; Skurtveit, Elin; Ando, Edward; Marinelli, Flavia; Viggiani, G.; Dal Pont, S.; Braathen, Alvar; Hovland, Beate; Bésuelle, P.; Alikarami, Reza; Zalmstra, Heleen & Sokoutis, Dimitrios (2015). Strain localization in sandstone and its implications for CO2 storage. First Break.  ISSN 0263-5046.  33(7), s 81- 92 Show summary

  Geological storage of CO2 is a key technical solution to the climate-energy challenge, but it has a number of technological constraints (Baines and Worden 2004; Halland et al., 2011), broadly under the themes of assuring adequate storage capacity and long-term storage integrity. A suitable CO2-storage reservoir should consist of rock formations with sufficient porosity, permeability and connectivity in order to provide an adequate storage volume. The role of faults and their associated deformation structures (such as deformation bands and fractures) in controlling both storage capacity and long-term storage integrity is thus a key factor in achieving globally significant CO2 storage (Figure 1). Although some sedimentary basins on the Norwegian continental shelf already harbour operational CO2- injection and storage projects such as Sleipner (Zweigel et al., 2004) and Snøhvit (Hansen et al., 2013), our understanding of reservoir fluid communication due to compartmentalization is far from complete and will be important for further use of the offshore basins for CO2 storage. In addition to the inherited structural features, elevated injection pressures may cause hydraulic fractures or stimulate fault reactivation which both point to the need to characterize the geomechanical response of the rock system to CO2 injection (Rutqvist, 2012; Iding and Ringrose, 2010). In the present work, we investigate the effects of faults and their related structures on the geomechanical and petrophysical properties of sandstone reservoirs. Important components of fault systems include fractures and deformation bands in the damage zone and fault core (Caine et al., 1996; Shipton and Cowie, 2003; Fossen et al., 2007). Fault systems may enhance or suppress fluid communication, which in turn may affect the storage capacity and conductivity of the candidate reservoirs (Figure 1). As a case study, a reservoir model of the Tubåen Formation at the Snøhvit CO2 injection site in the Barents Sea (Grude et al., 2013; Hansen et al., 2013) was investigated using 4D seismic data and fault attribute analysis. The characteristics of deformation structures (e.g. sub-seismic faults, deformation bands and fractures) were investigated by field studies of outcrop analogues and by triaxial laboratory experiments to provide a basis for numerical modelling. Fault architecture within reactivated fault systems was studied by the use of analogue modelling. Key questions addressed in the work include: a) Where and when might strain localize in the reservoir? b) How does rock strain influence fluid communication? c) How might structural architecture affect CO2 storage effectiveness?

• Gabrielsen, Roy; Fossen, Haakon; Faleide, Jan Inge & Hurich, Charles A. (2015). Mega-scale Moho relief and the structure of the lithosphere on the eastern flank of the Viking Graben, offshore southwestern Norway. Tectonics.  ISSN 0278-7407.  34(5), s 803- 819 . doi: 10.1002/2014TC003778
• Gabrielsen, Roy; Nystuen, Johan Petter; Jarsve, Erlend Morisbak & Lundmark, Anders Mattias (2015). The Sub-Cambrian Peneplain in southern Norway: Its geological significance and its implications for post-Caledonian faulting, uplift and denudation. Journal of the Geological Society.  ISSN 0016-7649.  172(6), s 777- 791 . doi: 10.1144/jgs2014-154
• Jarsve, Erlend Morisbak; Eidvin, Tor; Nystuen, Johan Petter; Faleide, Jan Inge; Gabrielsen, Roy & Thyberg, Brit Inger (2015). The oligocene succession in the Eastern North Sea: Basin development and depositional systems. Geological Magazine.  ISSN 0016-7568.  152(4), s 668- 693 . doi: 10.1017/S0016756814000570
• Lundmark, Anders Mattias; Pozer Bue, Edina; Gabrielsen, Roy H.; Flaat, Kjersti; Strand, Tor & Ohm, Sverre Ekrene (2015). Provenance of late Palaeozoic terrestrial sediments on the northern flank of the Mid North Sea High: detrital zircon geochronology and rutile geochemical constraints. Geological Society Special Publication.  ISSN 0305-8719.  386(1), s 243- 259 . doi: 10.1144/SP386.4
• Skurtveit, Elin; Grande, Lars; Ogebule, Oluwakemi Yetunde; Gabrielsen, Roy; Faleide, Jan Inge; Mondol, Nazmul Haque; Maurer, R. & Horsrud, Per (2015). Mechanical testing and sealing capacity of the Upper Jurassic Draupne Formation, North Sea, In Peter Smeallie (ed.),  49th US Rock Mechanics/Geomechanics Symposium - ARMA.  American Rock Mechanics Association (ARMA).  ISBN 978 0 9794975 0 6.  ARMA 15-331.
• Bastesen, Eivind; Rotevatn, Atle; Braathen, Alvar; Gabrielsen, Roy; Dypvik, Henning & Kalleson, Elin (2014). Polyphasal brecciation history revealing the nature and depth of Caledonian contractional deformation in the outboard terranes of West Central Norway. Norsk Geologisk Tidsskrift.  ISSN 0029-196X.  93, s 215- 228
• Fossen, Haakon; Gabrielsen, Roy; Faleide, Jan Inge & Hurich, Charles A. (2014). Crustal stretching in the Scandinavian Caledonides as revealed by deep seismic data. Geology.  ISSN 0091-7613.  42(9), s 791- 794 . doi: 10.1130/G35842.1
• Gabrielsen, Roy & Braathen, Alvar (2014). Models of fracture lineaments - Joint swarms, fracture corridors and faults in crystalline rocks, and their genetic relations. Tectonophysics.  ISSN 0040-1951.  628, s 26- 44 . doi: 10.1016/j.tecto.2014.04.022
• Jarsve, Erlend Morisbak; Faleide, Jan Inge; Gabrielsen, Roy & Nystuen, Johan Petter (2014). Mesozoic and Cenozoic basin configurations in the North Sea, In Allard W. Martinius; Rodmar Ravnås; John A. Howell; Ronald J. Steel & J. P. Wonham (ed.),  From Depositional Systems to Sedimentary Successions on the Norwegian Continental Margin.  Wiley-Blackwell.  ISBN 9781118920466.  Chapter 15.  s 417 - 452
• Jarsve, Erlend Morisbak; Krøgli, Svein Olav; Etzelmuller, Bernd & Gabrielsen, Roy (2014). Automatic identification of topographic surfaces related to the sub-Cambrian peneplain (SCP) in southern Norway - Surface generation algorithms and implications. Geomorphology.  ISSN 0169-555X.  211, s 89- 99 . doi: 10.1016/j.geomorph.2013.12.032
• Jarsve, Erlend Morisbak; Maast, Tom Erik; Gabrielsen, Roy; Faleide, Jan Inge; Nystuen, Johan Petter & Sassier, Caroline (2014). Seismic stratigraphic subdivision of the Triassic succession in the Central North Sea; integrating seismic reflection and well data. Journal of the Geological Society.  ISSN 0016-7649.  171(3), s 353- 374 . doi: 10.1144/jgs2013-056
• Baig, Irfan; Aagaard, Per; Sassier, Caroline; Faleide, Jan Inge; Jahren, Jens; Gabrielsen, Roy H.; Fawad, Manzar; Nielsen, Lars Henrik; Kristensen, Lars & Bergmo, Per Eirik Strand (2013). Potential Triassic and Jurassic CO2 Storage Reservoirs in the Skagerrak-Kattegat Area. Energy Procedia.  ISSN 1876-6102.  37, s 5298- 5306 . doi: 10.1016/j.egypro.2013.06.447 Full text in Research Archive. Show summary

  Regional assessment studies for CO2 storage plays have been carried out in the Norwegian-Danish Basin of the Central North Sea and in the Skagerrak-Kattegat area. The development of the reservoir models is a part of an ongoing interdisciplinary project with the overall goal to establish a basis for large-scale handling of CO2 in this area, including regional CO2 source and capture possibilities, transportation and infrastructure, possible storage sites as well as legal aspects relating to the whole CCS chain. The study shows that all the necessary premises for a safe, long term CO2 storage, are present in the area. Two trap types for storage have been studied more closely: 1) large gently inclined, unfaulted reservoirs in the northern Skagerrak area and 2) dome structures with four-way closures above salt pillows in the Norwegian Danish Basin. We have closely focused on the Upper Triassic-lowermost Jurassic Gassum Formation and the Middle Jurassic Haldager Sand Formation. The current study presents reservoir characteristics of the sandstones of the Gassum and Haldager formations in the Fjerritslev Trough and on the Skagerrak-Kattegat Platform.

• Blinova, Maria Konstantinovna; Faleide, Jan Inge; Gabrielsen, Roy H. & Mjelde, Rolf (2013). Analysis of structural trends of sub-seafloor strata in the Isfjorden area of the West Spitsbergen Fold-and-Thrust Belt based on multichannel seismic data. Journal of the Geological Society.  ISSN 0016-7649.  170(4), s 657- 668 . doi: 10.1144/jgs2012-109
• Midtkandal, Ivar; Brun, Jean-Pierre; Gabrielsen, Roy H. & Huismans, Ritske (2013). Control of lithosphere rheology on subduction polarity at initiation: Insights from 3D analogue modelling. Earth and Planetary Science Letters.  ISSN 0012-821X.  361, s 219- 228 . doi: 10.1016/j.epsl.2012.10.026
• Roffeis, Cornelia; Corfu, Fernando & Gabrielsen, Roy H. (2013). A Sveconorwegian terrane boundary in the Caledonian Hardanger-Ryfylke Nappe Complex: The lost link between Telemarkia and the Western Gneiss Region?. Precambrian Research.  ISSN 0301-9268.  228, s 20- 35 . doi: 10.1016/j.precamres.2013.01.008
• Skurtveit, Elin; Torabi, Anita; Gabrielsen, Roy H. & Zoback, Mark D. (2013). Experimental investigation of deformation mechanisms during shear-enhanced compaction in poorly lithified sandstone and sand. Journal of Geophysical Research (JGR): Solid Earth.  ISSN 2169-9313.  118(8), s 4083- 4100 . doi: 10.1002/jgrb.50342
• Blinova, Maria; Faleide, Jan Inge; Gabrielsen, Roy H. & Mjelde, Rolf (2012). Seafloor expression and shallow structure of a fold-and-thrust system, Isfjorden, west Spitsbergen. Polar Research.  ISSN 0800-0395.  31:11209 . doi: 10.3402/polar.v31i0.11209
• Lundmark, Anders Mattias; Gabrielsen, Roy H.; Austrheim, Håkon Olav; Flaat, Kjersti; Strand, Tor & Ohm, Sverre Ekrene (2012). Late Devonian rifting in the central North Sea: evidence from altered felsic volcanic rocks in the Embla oil field. Marine and Petroleum Geology.  ISSN 0264-8172.  29(1), s 204- 218 . doi: 10.1016/j.marpetgeo.2011.06.002
• Andersen, Tom; Saeed, Ayesha; Gabrielsen, Roy H. & Olaussen, Snorre (2011). Provenance characteristics of the Brumunddal sandstone in the Oslo Rift derived from U-Pb, Lu-Hf and trace element analyses of detrital zircons by laser ablation ICMPS. Norsk Geologisk Tidsskrift.  ISSN 0029-196X.  91(1-2), s 1- 18 Show summary

  The 800 m thick Brumunddal sandstone is partly an eolian, partly a fluvial sandstone deposited in a fault-bounded basin in the northern part of the Oslo Rift in Permian time.The sandstone is the youngest rift-related deposit in the northern part of the Oslo Rift. Well rounded detrital zircons are common accessory mineral grains in the sandstone. U-Pb dating of detrital zircon from a sample of the Brumunddal sandstone by LAM-ICPMS gives a range of ages from (rare) late Archaean ages to Permian (283 +/- 4 Ma). The age and initial epsilon Hf pattern of zircons in the sediment match the main rock- forming events in Fennoscandia from Archaean to Phanerozoic time. This kind of diverse provenance was most likely obtained by repeated recycling of clastic sediments of Fennoscandian origin, with Silurian, continental sandstones as the most probable direct precursors. Trace element distributions show a conspicuous absence of patterns with the high level of U and Th enrichment typical of zircon from granitic rocks. This is consistent with a complex transport and redepositional history: High U-Th, metamict zircons were selectively removed by abrasion during repeated transport-deposition-erosion cycles. In addition to recycled material. Caledonian syn-orogenic intrusions and Permian intermediate to felsic plutonic rocks in the Oslo Rift itself were minor, but still significant sources of detrital zircon.

• Leever, Karen Agneta; Gabrielsen, Roy H.; Faleide, Jan Inge & Braathen, Alvar (2011). A transpressional origin for the West Spitsbergen fold-and-thrust belt: Insight from analog modeling. Tectonics.  ISSN 0278-7407.  30 . doi: 10.1029/2010TC002753
• Leever, Karen Agneta; Gabrielsen, Roy H.; Sokoutis, Dimitrios & Willingshofer, Ernst (2011). The effect of convergence angle on the kinematic evolution of strain partitioning in transpressional brittle wedges: Insight from analog modeling and high-resolution digital image analysis. Tectonics.  ISSN 0278-7407.  30 . doi: 10.1029/2010TC002823
• Lundmark, Anders Mattias; Gabrielsen, Roy H. & Brown, John Flett (2011). Zircon U-Pb age for the Orkney lamprophyre dyke swarm, Scotland, and relations to Permo-Carboniferous magmatism in northwestern Europe. Journal of the Geological Society.  ISSN 0016-7649.  168(6), s 1233- 1236 . doi: 10.1144/0016-76492011-017
• Lundmark, Anders Mattias; Gabrielsen, Roy H. & Flett Brown, John (2011). Zircon U–Pb age for the Orkney lamprophyre dyke swarm, Scotland, and relations to Permo-Carboniferous magmatism in northwestern Europe. Journal of the Geological Society.  ISSN 0016-7649.  168, s 1233- 1236 . doi: 10.1144/0016-76492011-017

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• Gabrielsen, Roy Helge & Lacasse, Suzanne (2016). Natural disasters and societal safety. Det Norske Videnskaps-Akademi.  ISBN 82-7719-083-2.  173 s.
• Gabrielsen, Roy Helge (2015). The Structure and Hydrocarbon Traps in Sedimentary Basins. Springer Publishing Company.  ISBN 978-3-642-34131-1.  41 s.
• Gabrielsen, Roy H. & Grue, John (2012). Norwegian Energy Policy in Context of the Global Energy Situation. Novus Forlag.  ISBN 978-82-7099-705-3.  129 s. Show summary

  The symposium was held in the House of the Academy (DNVA) in Oslo on 1st February, 2012 and had 150 participants. His Majesty King Harald V attended the complete meeting. Ola Borten Moe, Minister of Petroleum and Energy, gave the intro­ductory talk. He was followed by CEO Helge Lund of Statoil and CEO Christian Rynning-Tønnesen of Statkraft. Experts invited by the learned societies contributed with talks on: the transition from conventional to renewable energy, the power-intensive metallurgical industry, and challenges in energy and climate policy. The volume includes a chapter on energy efficiency that has been added after the symposium.

• Grue, John & Gabrielsen, Roy H. (ed.) (2011). Marine Transport in the High North. Novus Forlag.  ISBN 978-82-7099-641-4.  124 s.

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• Hassaan, Muhammad; Faleide, Jan Inge; Gabrielsen, Roy Helge & Tsikalas, Filippos (2020). Anatomy of the evaporite accumulation and salt wall evolution in Tiddlybanken Basin, southeastern Norwegian Barents Sea.
• Hassaan, Muhammad; Faleide, Jan Inge; Gabrielsen, Roy Helge & Tsikalas, Filippos (2020). Control of Carboniferous basinal evolution on evaporite accumulations and salt structures dynamics in the southeastern Norwegian Barents Sea.
• Hassaan, Muhammad; Faleide, Jan Inge; Gabrielsen, Roy Helge & Tsikalas, Filippos (2020). Pre-salt Carboniferous basin architecture, salt tectonics and basin modelling in the Nordkapp Basin and adjacent parts of the SE Norwegian Barents Sea.
• Hassaan, Muhammad; Faleide, Jan Inge; Gabrielsen, Roy Helge & Tsikalas, Filippos (2020). Pre-salt Carboniferous basin architecture, salt tectonics and basin modelling in the Nordkapp Basin, SW Barents Sea.
• Hassaan, Muhammad; Faleide, Jan Inge; Gabrielsen, Roy Helge & Tsikalas, Filippos (2019). Anatomy of the evaporite accumulation and salt wall evolution in Tiddlybanken Basin, southeastern Norwegian Barents Sea..
• Hassaan, Muhammad; Faleide, Jan Inge; Gabrielsen, Roy Helge & Tsikalas, Filippos (2019). Carboniferous Graben Structures, Evaporite Accumulations and Inversion in the Southeastern Norwegian Barents Sea. Show summary

  2D regional seismic reflection profiles and well data are used for the investigation of the deep basin architecture in the southeastern Norwegian Barents Sea. The study area contains thick upper Paleozoic to Mesozoic sedimentary strata with prominent structural features comprising the Haapet, Veslekari, and Signalhorn Domes; the Tiddlybanken Basin, Fedynsky High, and eastern Finnmark Platform. Interpretation of selected seismic profiles and time structure maps are presented focusing on the positions, extent, and configurations of the Carboniferous basins. Furthermore, we investigate the relation between the Carboniferous graben structures, evaporites accumulations and inversion in the area. The basin boundary faults of the Carboniferous structures strike NW-SE, and the syn-rift Carboniferous sequences were deposited in half and full grabens. Basins are separated by platforms and structural highs, while basin infill generally dips towards the axis of the grabens, except for the half-graben on the Finnmark Platform where strata dip towards the north and the half-grabens beneath the Haapet Dome where strata dip to the south. In the study area, evaporites are accommodated in the Carboniferous basins and carbonates occupy the structural highs. The deposition of evaporites was constrained by the master faults of the grabens, except for an evaporitic body, which oversteps the rift margins and connects with the southeastern and central parts of the Nordkapp Basin. Furthermore, a thick Triassic succession, with provenance mainly in the southeast, was deposited in the region, while thin Jurassic sediments outcrop at seafloor over the Veslekari Dome and the salt diapir of the Tiddlybanken Basin. Prograding Cretaceous strata mark another phase of regional subsidence in the study area. Several domes are identified in the near base Triassic to the base Cretaceous levels with different shapes, orientation and sizes. The distribution and evolution of the younger domes are partially controlled by the deep-seated Carboniferous structures. Distinct observations including the lateral thickness variations for the uppermost Triassic to the lowermost Cretaceous sediments, the rim syncline development and the onlap at various stratigraphic levels all suggest several phases of doming. We propose a Paleogene timing for the main phase of reactivation of the inverted domes due to Carboniferous graben structures, probably in response to regional compressional stresses.

• Hassaan, Muhammad; Faleide, Jan Inge; Gabrielsen, Roy Helge & Tsikalas, Filippos (2019). Carboniferous graben structures, evaporite accumulations and tectonic inversion in southeastern Norwegian Barents Sea.. Show summary

  Improved resolution reprocessed 2D multi-channel seismic reflection profiles, combined with exploration wells and stratigraphic boreholes penetrating upper Paleozoic sequences on the eastern Finnmark Platform were utilized particularly to analyse the Carboniferous graben system, evaporite bodies distribution, domes and salt wall in the southeastern Norwegian Barents Sea and east Finnmark Platform. Seven deep-seated Carboniferous grabens, not previously described and named, were defined and informally named as grabens G1-G7. Five evaporite bodies, named EB1-EB5, have been mapped in detail. During late Devonian, the study area was dominated by a central structural high region (Fedynsky High) rimmed by sag basins to the north and south it. We suggest that late Devonian-early Carboniferous (Mississippian) NE-SW oriented stress regime as suggested for the evolution of the Pechora Basin, eastern Barents Sea, and Olga-Sørkapp region also created the NW-SE striking graben structures (G1-G5) in the southeastern Norwegian Barents Sea, mainly exploiting the Timanian Orogen structural grain. In the early Pennsylvanian, the NE-SW trending Nordkapp Basin dissected the already existing G6 and G7 grabens. Pennsylvanian to early Permian evaporite units were deposited. The temporal relationship suggests that the evaporites were deposited as post-rift sequences within the Carboniferous grabens of the southeastern Norwegian Barents Sea and as syn-rift or early post-rift sequences within the Nordkapp Basin. The discrepancy in syn-rift to post-rift basin conditions affected the distribution and thickness of the accumulated evaporites, partly or fully occupying the available accommodation space. Evaporite bodies EB1, EB3, and EB5 are correlated to the Gipsdalen Group halite and non-halite lithologies (i.e. anhydrite-related compositions) with less thickness, while evaporite body EB4 contained mobile halite lithology and EB2 comprised of transitional lithology from graben margin (non-mobile) to the center (mobile). The deep-seated structures constrained the accumulation and facies variations of the evaporites and strongly controlled the distribution and partially the evolution of the stratigraphically shallower domes. The effect of salt mobilization on the dome evolution depended on the relative amount of lithologies with mobile to immobile properties, and the relative stratigraphic thickness of each unit. The NW-SE trending salt wall evolution is complex, varies along-strike, and has affected the structural development of the Signalhorn Dome that was instigated during late Triassic due to the far-field stresses from the evolving Novaya Zemlya fold-and-thrust belt. The Haapet, Veslekari, Alpha and Beta domes were instigated and the salt wall was rejuvenated during late Triassic due to compressional stresses propagating from the Novaya Zemlya fold-and-thrust belt as these structures were located in the relative proximity. Several studies on the Barents Sea-Svalbard region have similarly recorded the results of far-field compressional stresses attributed to the Novaya Zemlya fold-and-thrust belt. All of the structural elements were mildly reactivated during upper Jurassic and earliest Cretaceous. However, the exact causes of this reactivation are difficult to be deciphered in detail due to lack of dense seismic reflection coverage and relatively poor seismic resolution in the southeastern Norwegian Barents Sea. Prograding shelf platform complex sediments during early Cretaceous buried the domes and the salt wall until reactivation of the deep-seated Carboniferous grabens led to the reactivation of these structures and to the erosion of the post-lower Cretaceous strata over their crest. We infer an early-middle Eocene timing for the main phase of reactivation of the domes and salt wall, probably in response to regional compressional stresses related to the transpressional Eurekan/Spitsbergen orogeny

• Hassaan, Muhammad; Faleide, Jan Inge; Gabrielsen, Roy Helge & Tsikalas, Filippos (2019). Control of Carboniferous Graben Structures on Evaporite Accumulation and Domes Location in Southeastern Norwegian Barents Sea. Show summary

  We utilize available seismic and well data, and focus on the distribution, orientation of deep-seated Carboniferous graben structures and their control on the domes in the southeastern Norwegian Barents Sea. We map prominent NW-SE trending that represents Timanian Orogeny trend, deep-seated Carboniferous graben structures separated by platforms and structural highs. Evaporites were accumulated in the deep basins, while carbonates occupied the highs. Several distinct domes at top Gipsdalen to Cretaceous levels are present within the study area, including the Haapet, Veslekari, and Signalhorn domes, and the central domal feature of the Fedynsky High. The spatial analysis of graben structures, evaporite accumulation, and domes reveal that the deep-seated Carboniferous structures strongly control the distribution and partially the evolution of the domes along with facies variations. Effect of salt mobilization on the dome evolution is dependent on the lithological variations (mobile and immobile evaporites and carbonates) and thickness. Lateral thickness variations of the uppermost Triassic to the lowermost Cretaceous sediments, the Cretaceous onlaps to the Jurassic successions and erosion of the residual Cretaceous strata, all suggest a multiphase evolution of the domes. We propose Paleogene timing for the main phase of reactivation of the domes, probably in response to regional compressional stresses.

• Hassaan, Muhammad; Faleide, Jan Inge; Gabrielsen, Roy Helge & Tsikalas, Filippos (2019). Deep-seated Carboniferous graben structures and reactivation of younger domes in the southeastern Norwegian Barents Sea. Show summary

  2D regional seismic reflection profiles and well data were used for the mapping of the deep Carboniferous basin architecture in the southeastern Norwegian Barents Sea. Interpretation of selected seismic profiles and time structure maps are presented focusing on the positions, configurations and deformation stages of these basins. Furthermore, we investigate the connection between the Carboniferous graben structures, evaporites accumulations and reactivation of the younger domes in the area. The basin boundary faults and affiliated depo-centers of the Carboniferous structures strike NW-SE, defining structural configurations consisting of half- and full grabens. The basins are separated by platforms and structural highs. The basin fill generally dips towards the axis of the grabens, except for the half-graben on the Finnmark Platform, where strata dip towards the north and the half-grabens beneath the Haapet Dome where strata dip to the south. Evaporites are accommodated in the Carboniferous basins and carbonates occupy the structural highs. The deposition of evaporites was constrained by the master faults of the grabens, except for one evaporite body, which oversteps the rift margins and connects with the southeastern and central parts of the Nordkapp Basin. Several domes are identified at the near base Triassic to the base Cretaceous levels. These have different shapes, orientation and sizes. The distribution and evolution of the younger domes are partially controlled by the deep-seated Carboniferous structures. Lateral thickness variations for the uppermost Triassic to the lowermost Cretaceous sediments, the rim syncline development and the onlap at various stratigraphic levels, all suggest several phases of doming. We propose a Paleogene timing for the main phase of reactivation of the domes due to Carboniferous graben structures, probably in response to regional compressional stresses.

• Gabrielsen, Roy Helge (2018). Sum up and looks into the future.
• Hassaan, Muhammad; Faleide, Jan Inge; Gabrielsen, Roy Helge & Tsikalas, Filippos (2018). Correlation between the Carboniferous graben structures, salt accumulations and inversion in the southeastern Norwegian Barents Sea.
• Gabrielsen, Roy Helge; Faleide, Jan Inge; Wong, P.W; Gac, Sebastien; Indrevær, Kjetil; Faisal Miraj, M.; Dinkgreve, Patricia; Sokoutis, Dimitrios & Pascal, Christophe (2017). Palaeogene North Atlantic opening along the Barents Sea margin and its adjacent deformation.
• Gac, Sebastien; Indrevær, Kjetil; Gabrielsen, Roy Helge & Faleide, Jan Inge (2017). A model of the tectonic evolution of the Loppa High from Late Paleozoic to present-day.
• Indrevær, Kjetil; Gabrielsen, Roy Helge; Bugge, Aina Juell & Faleide, Jan Inge (2017). Latest Permian/earliest Triassic folds & thrusts on the Loppa High..
• Indrevær, Kjetil; Gabrielsen, Roy Helge; Gac, Sebastien & Faleide, Jan Inge (2017). Is there a tectonic signal in the development of the late Palaeozoic bioherms on the Loppa High?.
• Indrevær, Kjetil; Gac, Sebastien; Gabrielsen, Roy Helge & Faleide, Jan Inge (2017). Can metamorphic phase changes in the lower crust help explain the repeated uplift and subsidence of the Loppa High area through time?.
• Gabrielsen, Roy Helge; Sokoutis, Dimitrios; Willingshofer, Ernst & Faleide, Jan Inge (2016). Experiments on horizontal and vertical fault linkage and its relevance for the Hoop Fault Complex.
• Faleide, Jan Inge; Planke, Sverre; Abdelmalak, Mohamed Mansour; Zastrozhnov, Dmitrii; Wong, P.W.; Shephard, Grace; Indrevær, Kjetil; Tsikalas, Filippos; Gabrielsen, Roy Helge; Gernigon, Laurent; Blaich, Olav A. & Myklebust, Reidun (2016). Basin architecture and evolution at NE Atlantic conjugate margins.
• Gabrielsen, Roy Helge; Braathen, Alvar; Faleide, Jan Inge; Indrevær, Kjetil & Aamodt, L (2016). The Feda‐Lista‐Bredtflå fault system; a major lineament crossing the offshore‐onshore transition.
• Gabrielsen, Roy Helge & Nystuen, Johan Petter (2016). Glacial striations from the Varangerian glaciation in South Norway.
• Indrevær, Kjetil; Faleide, Jan Inge; Sæbø Serck, Christopher & Gabrielsen, Roy Helge (2016). Paleohighs of the western Barents Sea and their onshore correlation.
• Gabrielsen, Roy & Sokoutis, Dimitrios (2015). Fault initiation, fault growth and fault linkage; Musings from analogue experiments.
• Faleide, Jan Inge; Bjørlykke, Knut & Gabrielsen, Roy Helge (2015). Geology of the Norwegian Continental Shelf, In Knut Bjørlykke (ed.),  Petroleum Geoscience. From sedimentary environments to rock physics - second edition.  Encyclopedia of Global Archaeology/Springer Verlag.  ISBN 978-3-642-34131-1.  Chapter 25.  s 603 - 636
• Faleide, Jan Inge; Gabrielsen, Roy Helge; Indrevær, Kjetil; Gac, Sebastien; Minakov, Aleksander; Miraj, M.F. & Pascal, Christophe (2015). Contractional events in the Barents Sea basin evolution - timing, causes and implications.
• Faleide, Jan Inge; Kalani, Mohsen; Sassier, Caroline; Angeli, Matthieu; Ogebule, Oluwakemi Yetunde; Baig, Irfan; Jarsve, Erlend M.; Gabrielsen, Roy Helge; Mondol, Nazmul Haque; Jahren, Jens; Aagaard, Per; Skurtveit, Elin; Grande, Lars; Maurer, Rudolf & Horsrud, P. (2015). Caprock research in the CO2Seal project.
• Faleide, Jan Inge; Mahajan, Aatisha; Gabrielsen, Roy Helge; Breivik, Asbjørn Johan; Planke, Sverre & Myklebust, Reidun (2015). Basement and Late Paleozoic basin configurations in the western and central Barents Sea.
• Faleide, Jan Inge; Wong, Po Wan; Gabrielsen, Roy Helge; Tsikalas, Filippos; Blaich, Olav Antonio; Planke, Sverre & Myklebust, Reidun (2015). Basin evolution at the SW Barents Sea margin and its conjugate off NE Greenland.
• Gabrielsen, Roy & Braathen, Alvar (2015). Dynamics, Architecture and Influences on Fluid Flow in Normal Faults.
• Indrevær, Kjetil; Faleide, Jan Inge; Gabrielsen, Roy Helge; Mulrooney, Mark & Braathen, Alvar (2015). Inversion along the Troms-Finnmark Fault Complex, SW Barents Sea: Structural character and timing.
• Faleide, Jan Inge; Wong, P.W.; Gabrielsen, Roy; Tsikalas, Filippos; Blaich, Olav A.; Planke, Sverre & Myklebust, Reidun (2014). Basin evolution at the SW Barents Sea margin and its conjugate off NE Greenland.
• Gabrielsen, Roy H.; Jarsve, Erlend Morisbak; Lundmark, Anders Mattias; Nystuen, Johan Petter & Faleide, Jan Inge (2014). The evolution of the passive continental margin of Norway and its adjacent mainland – using the sub-Cambrian peneplain as a reference surface.
• Gabrielsen, Roy; Braathen, Alvar & Skar, Tore (2014). Normal Faults in Sedimentary Rocks; Dynamics, Architecture and Influences on Fluid Flow.
• Lundmark, Anders Mattias; Kristoffersen, Magnus; Thomsen, T; Gillhespy, Lewis & Gabrielsen, Roy H. (2014). Revealing hidden parts of the Caledonian orogen by provenance analysis of Mesozoic sandstones.
• Mahajan, Aatisha; Gabrielsen, Roy & Faleide, Jan Inge (2014). Structural analysis of 3D seismic for Hoop Fault Complex, SW Barents Sea.
• Miraj, M.A.F.; Pascal, C.; Gabrielsen, Roy & Faleide, Jan Inge (2014). Numerical modeling of main inverted structures in the western Barents Sea.
• Sassier, Caroline; Jarsve, Erlend Morisbak; Heeremans, Michel; Abdelmalak, Mohamed Mansour; Faleide, Jan Inge & Gabrielsen, Roy (2014). Salt distribution in the Norwegian-Danish Basin, Central North Sea.
• Baig, Irfan; Aagaard, Per; Fawad, Manzar; Sassier, Caroline; Faleide, Jan Inge; Jahren, Jens; Gabrielsen, Roy H.; Nielsen, Lars Henrik; Kristensen, Lars & Bergmo, Per Eirik Strand (2013). Reservoir Characterization of Potential Triassic and Jurassic Reservoirs for CO2 Storage in the Skagerrak-Kattegat Area.
• Gabrielsen, Roy H.; Aam, Sverre; Bendiksen, Kjell Hugo; Faanes, Hans Haakon; Hope, Einar; Rytter, Erling; Åm, Knut; Killingtveit, Ånund & Johnson, Hein (ed.) (2013). A National Energy Strategy 1913-1917.
• Lundmark, Anders Mattias; Kristoffersen, Magnus & Gabrielsen, Roy H. (2013). Heavy mineral signatures of Lunde, Statfjord, Nansen and Cook Formation sands, northern North Sea – constraints on origins, mixing patterns and post-depositional alteration.
• Sassier, Caroline; Jarsve, Erlend Morisbak; Baig, Irfan; Heeremans, Michel; Faleide, Jan Inge; Gabrielsen, Roy H. & Aagaard, Per (2013). Salt Tectonics in the Norwegian-Danish Basin - Implications on trap and depositional systems.
• Theissen-Krah, Sonja; Schmid, Daniel Walter; Faleide, Jan Inge; Planke, Sverre; Gabrielsen, Roy H. & Myklebust, Reidun (2013). Structural and thermal reconstruction of a transect across the More Basin.
• Theissen-Krah, Sonja; Schmid, Daniel Walter; Faleide, Jan Inge; Planke, Sverre; Gabrielsen, Roy H. & Myklebust, Reidun (2013). Structure and evolution of the Møre Basin – mid-Norwegian continental margin.
• Baig, Irfan; Aagaard, Per; Fawad, Manzar; Sassier, Caroline; Faleide, Jan Inge; Jahren, Jens; Gabrielsen, Roy H.; Nielsen, Lars & Bergmo, Per Eirik Strand (2012). Potential Triassic and Jurassic CO2 storage reservoirs in the Skagerrak area.
• Baig, Irfan; Aagaard, Per; Sassier, Caroline; Faleide, Jan Inge; Jahren, Jens; Gabrielsen, Roy H.; Fawad, Manzar; Nielsen, Lars Henrik; Kristensen, Lars & Bergmo, Per Eirik Strand (2012). Potential Triassic and Jurassic CO2 storage reservoirs in the Skagerrak-Kattegat area.
• Bastesen, Eivind; Dypvik, Henning; Gabrielsen, Roy H.; Braathen, Alvar; Kalleson, Elin & Rotevatn, Atle (2012). Enigmatic breccia at Frøya (Mid Norway) – Impact, fault or fluidization breccia?.
• Grue, John & Gabrielsen, Roy H. (2012). Introduction - The Norwegian Energy System and the Global Perspective, In  Norwegian Energy Policy in Context of the Global Energy Situation.  Novus Forlag.  ISBN 978-82-7099-705-3.  Innledning.  s 13 - 19
• Sassier, Caroline; Jarsve, Erlend Morisbak; Kalani, Mohsen; Heeremans, Michel; Faleide, Jan Inge; Aagaard, Per & Gabrielsen, Roy H. (2012). Effects of salt tectonics on potential CO2 reservoir and caprock in the Norwegian-Danish Basin.
• Thorsen, Thor Axel & Gabrielsen, Roy H. (2012). Cooperation between Academia and Industry; Solving Problems of Common Interest.
• Braathen, Alvar; Gabrielsen, Roy & Bastesen, Eivind (2011). Analysis of extensional fault cores – Fault Facies characteristics of slip-surfaces and rock lenses.
• Faleide, Jan Inge; Clark, Steven S.; Glørstad-Clark, Evy; Gabrielsen, Roy H.; Nystuen, Johan Petter & Planke, Sverre (2011). Basin development and potential petroleum plays in he Central Barents Sea. NGF abstracts and proceedings.  (1), s 23- 24
• Gabrielsen, Roy H.; Jarsve, Erlend M. & Krøgli, S.O. (2011). An old unconformity rejuvenated: The sub-Cambrian peneplain in southern Norway. NGF abstracts and proceedings.  (1), s 29- 30
• Kjemperud, Magnus; Gabrielsen, Roy H.; Færseth, Roald B.; Tveranger, Jan & Buckley, Steven (2011). Fault architecture and reactivaed extensional faults in Carboniferous sediments, Northumberland, Great Britain. Abstracts and Proceedings of the Geological Society of Norway.  (1), s 49- 50
• Lundmark, Anders Mattias; Bue, Edina Pozer; Gabrielsen, Roy H.; Flaat, Kjersti; Strand, Tor & Ohm, Sverre Ekrene (2011). Provenance of Palaeozoic terrestrial sediments in the proto-Central Graben, Mid North Sea High: detrital zircon geochronology and rutile geochemical constraints.
• Lundmark, Anders Mattias; Kristoffersen, Magnus & Gabrielsen, Roy H. (2011). Provenance and reservoir heterogeneity in the Banks Group, northern North Sea.
• Midtkandal, Ivar; Gabrielsen, Roy H.; Brun, Jean-Pierre & Huismans, Ritske (2011). Modellling compression along a previously extended plate boundary; subduction vs. Obduction along the Iberian – Eurasian margin. Abstracts and Proceedings of the Geological Society of Norway.  (1), s 62- 62
• Valdresbråten, M.L.R; Gabrielsen, Roy H.; Færseth, Roald B.; Tveranger, Jan & Buckley, Steven (2011). Fault lenses and fracture frequencies in extensional faults affecting sandstone, Northumberland, Great Britain. Abstracts and Proceedings of the Geological Society of Norway.  (1), s 106- 107

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