Hostname: page-component-78c5997874-94fs2 Total loading time: 0 Render date: 2024-11-19T07:12:45.342Z Has data issue: false hasContentIssue false
  • English
  • Français

Lower Cretaceous Barents Sea strata: epicontinental basin configuration, timing, correlation and depositional dynamics

Published online by Cambridge University Press:  16 September 2019

Ivar Midtkandal Open the ORCID record for Ivar Midtkandal [Opens in a new window] ,
Jan Inge Faleide ,
Thea Sveva Faleide ,
Christopher Sæbø Serck ,
Sverre Planke Open the ORCID record for Sverre Planke [Opens in a new window] ,
Romain Corseri ,
Myrsini Dimitriou  and
Johan Petter Nystuen
Ivar Midtkandal*
Affiliation:
Department of Geosciences, University of Oslo, Oslo, Norway
Jan Inge Faleide
Affiliation:
Department of Geosciences, University of Oslo, Oslo, Norway Centre for Earth Evolution and Dynamics (CEED), University of Oslo, Oslo, Norway
Thea Sveva Faleide
Affiliation:
Department of Geosciences, University of Oslo, Oslo, Norway
Christopher Sæbø Serck
Affiliation:
Department of Geosciences, University of Oslo, Oslo, Norway
Sverre Planke
Affiliation:
Centre for Earth Evolution and Dynamics (CEED), University of Oslo, Oslo, Norway Volcanic Basin Petroleum Research AS, Oslo Science Park, Oslo, Norway
Romain Corseri
Affiliation:
Volcanic Basin Petroleum Research AS, Oslo Science Park, Oslo, Norway
Myrsini Dimitriou
Affiliation:
Equinor Energy AS, Forus Vest, Svanholmen 8, 4313Sandnes, Norway
Johan Petter Nystuen
Affiliation:
Department of Geosciences, University of Oslo, Oslo, Norway
*
Author for correspondence: Ivar Midtkandal, Email: [email protected]
Get access Rights & Permissions [Opens in a new window]

Abstract

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-wavelength tectonic tilt related to the Early Cretaceous High Arctic Large Igneous Province (HALIP) set up a fluvial system that developed from a sediment source area in the NW, which flowed SE across the Svalbard archipelago, terminating in a low-accommodation shallow sea within the Bjarmeland Platform area of the present-day Barents Sea. The basin deepened to the SE with a ramp-like basin floor with gentle dip. Seismic data show sedimentary lobes with internal clinoform geometry that advanced from the NW. These lobes interfingered with, and were overlain by, another younger depositional system with similar lobes sourced from the NE. The integrated data allow mapping of architectural patterns that provide information on basin physiography and control factors on source-to-sink transport and depositional patterns within the giant epicontinental basin. The results highlight how low-gradient, low-accommodation sediment transport and deposition has taken place along proximal to distal profiles for several hundred kilometres, in response to subtle changes in base level and by intra-basinal highs and troughs. Long-distance correlation along depositional dip is therefore possible, but should be treated with caution to avoid misidentification of timelines for diachronous surfaces.

Keywords

Barents SeaCretaceousclinoformssource-to-sinkpalaeogeography
Type
Original Article
Information
Geological Magazine , Volume 157 , Issue 3 , March 2020 , pp. 458 - 476
Copyright
© Cambridge University Press 2019

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Alvey, A, Gaina, C, Kusznir, NJ and Torsvik, TH (2008) Integrated crustal thickness mapping and plate reconstructions for the high Arctic. Earth and Planetary Science Letters 274, 310–21.CrossRefGoogle Scholar
Anfinson, OA, Leier, AL, Gaschnig, R, Embry, AF and Dewing, K (2012) U–Pb and Hf isotopic data from Franklinian Basin strata: insights into the nature of Crockerland and the timing of accretion, Canadian Arctic Islands (ed. M. Colpron). Canadian Journal of Earth Sciences 49, 1316–28.CrossRefGoogle Scholar
Antonsen, P, Elverhøi, A, Dypvik, H and Solheim, A (1991) Shallow bedrock geology of the Olga Basin area, northwestern Barents Sea. American Association of Petroleum Geologists Bulletin 75, 1178–94.Google Scholar
Århus, N (1991) The transition from deposition of condensed carbonates to dark claystones in the Lower Cretaceous succession of the southwestern Barents Sea. Norsk Geologisk Tidsskrift 71, 259–63.Google Scholar
Backman, J, Jakobsson, M, Frank, M, Sangiorgi, F, Brinkhuis, H, Stickley, C, O’Regan, M, Løvlie, R, Pälike, H, Spofforth, D, Gattacecca, J, Moran, K, King, J and Heil, C (2008) Age model and core-seismic integration for the Cenozoic Arctic Coring Expedition sediments from the Lomonosov Ridge. Paleoceanography 23(1), https://doi.org/10.1029/2007PA001476CrossRefGoogle Scholar
Blaich, OA, Tsikalas, F and Faleide, JI (2017) New insights into the tectono-stratigraphic evolution of the southern Stappen High and its transition to Bjørnøya Basin, SW Barents Sea. Marine and Petroleum Geology 85, 89–105.CrossRefGoogle Scholar
Buchan, KL and Ernst, RE (2018) A giant circumferential dyke swarm associated with the High Arctic Large Igneous Province (HALIP). Gondwana Research 58, 39–57.CrossRefGoogle Scholar
Bugge, T, Elvebakk, G, Fanavoll, S, Mangerud, G, Smelror, M, Weiss, HM, Gjelberg, J, Kristensen, SE and Nilsen, K (2002) Shallow stratigraphic drilling applied in hydrocarbon exploration of the Nordkapp Basin, Barents Sea. Marine and Petroleum Geology 19, 13–37.CrossRefGoogle Scholar
Cochran, JR, Edwards, MH and Coakley, BJ (2006) Morphology and structure of the Lomonosov Ridge, Arctic Ocean. Geochemistry, Geophysics, Geosystems 7.CrossRefGoogle Scholar
Cohen, KM, Finney, SC, Gibbard, PL and Fan, J-X (2013) The ICS International Chronostratigraphic Chart. Episodes 36, 199–204.CrossRefGoogle Scholar
Corfu, F, Polteau, S, Planke, S, Faleide, JI, Svensen, H, Zayoncheck, A and Stolbov, N (2013) U-Pb geochronology of Cretaceous magmatism on Svalbard and Franz Josef Land, Barents Sea large igneous province. Geological Magazine 150, 1127–35.CrossRefGoogle Scholar
Corseri, R, Faleide, TS, Faleide, JI, Midtkandal, I, Serck, CS, Trulsvik, M and Planke, S (2018) A diverted submarine channel of Early Cretaceous age revealed by high-resolution seismic data, SW Barents Sea. Marine and Petroleum Geology 98, 462–76.CrossRefGoogle Scholar
Cosgrove, GIE, Hodgson, DM, Poyatos-Moré, M, Mountney, NP and McCaffrey, WD (2018) Filter or conveyor? Establishing relationships between clinoform rollover trajectory, sedimentary process regime, and grain character within intrashelf clinothems, offshore New Jersey, U.S.A. Journal of Sedimentary Research 88, 917–41.CrossRefGoogle Scholar
Davidson, SK and North, CP (2009) Geomorphological regional curves for prediction of drainage area and screening modern analogues for rivers in the rock record. Journal of Sedimentary Research 79, 773–92.CrossRefGoogle Scholar
Dibner, VD (1998) Geology of Franz Josef Land. Norsk Polarinstitutt Meddelelser 146, 190.Google Scholar
Dibner, VD, Bro, EG, Preobrazhenskaya, EN, Pchelina, TM and Shkola, IV (1992) The geology of Franz Josef Land Archipelago, Russian Federation. In International Conference on Arctic Margins Proceedings (eds Solheim, A, Musatov, E and Heinz, N), p. 151. Anchorage: Norsk Polarinstututt Meddelelser.Google Scholar
Dimakis, P, Braathen, BI, Faleide, JI, Elverhøi, A and Gudlaugsson, ST (1998) Cenozoic erosion and the preglacial uplift of the Svalbard–Barents Sea region. Tectonophysics 300, 311–27.CrossRefGoogle Scholar
Dockman, DM, Pearson, DG, Heaman, LM, Gibson, SA and Sarkar, C (2018) Timing and origin of magmatism in the Sverdrup Basin, Northern Canada—Implications for lithospheric evolution in the High Arctic Large Igneous Province (HALIP). Tectonophysics 742–743, 50–65.CrossRefGoogle Scholar
Døssing, A, Jackson, HR, Matzka, J, Einarsson, I, Rasmussen, TM, Olesen, AV and Brozena, JM (2013) On the origin of the Amerasia Basin and the High Arctic Large Igneous Province-Results of new aeromagnetic data. Earth and Planetary Science Letters 363, 219–30.CrossRefGoogle Scholar
Drachev, SS, Malyshev, NA and Nikishin, AM (2010) Tectonic history and petroleum geology of the Russian Arctic Shelves: an overview. In Petroleum Geology: From Mature Basins to New Frontiers, pp. 591–619. Geological Society of London, Petroleum Geology Conference Series no. 7.Google Scholar
Drachev, S and Saunders, A (2006) The Early Cretaceous Arctic Lip: its geodynamic setting and implications for Canada Basin opening. In ICAM IV Proceedings (eds Scott, RA and Thurston, DK), pp. 216–23. Department of the Interior Minerals Management Service, Alaska Outer Continental Shelf Region, Dartmouth, Nova Scotia, Canada.Google Scholar
Dreyer, T, Corregidor, J, Arbues, P and Puigdefabregas, C (1999) Architecture of the tectonically influenced Sobrarbe deltaic complex in the Ainsa Basin, northern Spain. Sedimentary Geology 127(3–4), 127–69.CrossRefGoogle Scholar
Dypvik, H, Eikeland, TA, Backer-Owe, K, Andresen, A, Johansen, H, Elverhøi, A, Nagy, J, Haremo, P and Bjærke, T (1991a) The Janusfjellet Subgroup (Bathonian to Hauterivian) on central Spitsbergen: a revised lithostratigraphy. Polar Research 9, 21–44.CrossRefGoogle Scholar
Dypvik, H, Gudlaugsson, ST, Tsikalas, F, Attrep, M, Ferrell, RE, Krinsley, DH, Mørk, A, Faleide, JI and Nagy, J (1996) Mjølnir structure: An impact crater in the Barents Sea. Geology 24, 779–82.2.3.CO;2>CrossRefGoogle Scholar
Dypvik, H, Håkansson, E and Heinberg, C (2002) Jurassic and Cretaceous palaeogeography and stratigraphic comparisons in the North Greenland-Svalbard region. Polar Research 21, 91–108.CrossRefGoogle Scholar
Dypvik, H, Nagy, J, Eikeland, TA, Backer-Owe, K and Johansen, H (1991b) Depositional conditions of the Bathonian to Hauterivian Janusfjellet Subgroup, Spitsbergen. Sedimentary Geology 72, 55–78.CrossRefGoogle Scholar
Embry, AF (1992) Mesozoic stratigraphy of Franz Josef Land Archipelago, Arctic Russia—A literature review. Proceedings of the International Conference on Arctic Margins OCS Study MMS 94, Anchorage.Google Scholar
Embry, AF (1993) Crockerland-the northwest source area for the Sverdrup Basin, Canadian Arctic Islands. Arctic Geology and Petroleum Potential 2, 205–16.Google Scholar
Estrada, S, Mende, K, Gerdes, A, Gärtner, A, Hofmann, M, Spiegel, C, Damaske, D and Koglin, N (2018) Proterozoic to Cretaceous evolution of the western and central Pearya Terrane (Canadian High Arctic). Journal of Geodynamics 120, 45–76.CrossRefGoogle Scholar
Fagherazzi, S, Howard, AD, Niedoroda, AW and Wiberg, PL (2008) Controls on the degree of fluvial incision of continental shelves. Computers & Geosciences 34, 1381–93.CrossRefGoogle Scholar
Faleide, JI, Bjørlykke, K and Gabrielsen, RH (2015) Geology of the Norwegian Continental Shelf. In Petroleum Geoscience (ed Bjørlykke, K), pp. 467–499. Springer, Berlin.Google Scholar
Faleide, JI, Pease, V, Curtis, M, Klitzke, P, Minakov, A, Scheck-Wenderoth, M, Kostyuchenko, S and Zayonchek, A (2017) Tectonic implications of the lithospheric structure across the Barents and Kara shelves. In Circum-Arctic Lithosphere Evolution (eds Pease, V and Coakley, B), pp. 285–314. Geological Society of London, Special Publication no. 460.Google Scholar
Faleide, JI, Solheim, A, Fiedler, A, Hjelstuen, BO, Andersen, ES and Vanneste, K (1996) Late Cenozoic evolution of the western Barents Sea-Svalbard continental margin. Global and Planetary Change 12, 53–74.CrossRefGoogle Scholar
Faleide, JI, Tsikalas, F, Breivik, AJ, Mjelde, R, Ritzmann, O, Engen, O, Wilson, J and Eldholm, O (2008) Structure and evolution of the continental margin off Norway and the Barents Sea. Episodes 31, 82–91.CrossRefGoogle Scholar
Faleide, JI, Vågnes, E and Gudlaugsson, ST (1993) Late Mesozoic-Cenozoic evolution of the south-western Barents Sea in a regional rift-shear tectonic setting. Marine and Petroleum Geology 10, 186–214.CrossRefGoogle Scholar
Faleide, TS, Midtkandal, I, Planke, S, Corseri, R, Faleide, JI, Serck, CS and Nystuen, JP (2019) Characterisation and development of Early Cretaceous shelf platform deposition and faulting in the Hoop area, southwestern Barents Sea-constrained by high-resolution seismic data. Norwegian Journal of Geology 99, https://doi.org/10.17850/njg99-3-7CrossRefGoogle Scholar
Friedrich, AM, Bunge, H-P, Rieger, SM, Colli, L, Ghelichkhan, S and Nerlich, R (2018) Stratigraphic framework for the plume mode of mantle convection and the analysis of interregional unconformities on geological maps. Gondwana Research 53, 159–88, https://doi.org/10.1016/j.gr.2017.06.003CrossRefGoogle Scholar
Gabrielsen, RH, Grunnaleite, I and Ottesen, S (1993) Reactivation of fault complexes in the Loppa High area, southwestern Barents Sea. Norwegian Petroleum Society Special Publications 2, 631–41.CrossRefGoogle Scholar
Gac, S, Klitzke, P, Minakov, A, Faleide, JI and Scheck-Wenderoth, M (2016) Lithospheric strength and elastic thickness of the Barents Sea and Kara Sea region. Tectonophysics 691(A), 120–32.CrossRefGoogle Scholar
Gjelberg, J and Steel, RJ (1995) Helvetiafjellet formation (Barremian-Aptian), Spitsbergen: characteristics of a transgressive succession. Norwegian Petroleum Society Special Publications 5, 571–93.CrossRefGoogle Scholar
Gjelberg, J and Steel, R (2012) Depositional model for the Lower Cretaceous Helvetiafjellet Formation on Svalbard - diachronous vs. layer-cake models. Norsk Geologisk Tidsskrift 92, 41–53.Google Scholar
Glørstad-Clark, E, Birkeland, EP, Nystuen, JP, Faleide, JI and Midtkandal, I (2011) Triassic platform-margin deltas in the western Barents Sea. Marine and Petroleum Geology 28, 1294–314.CrossRefGoogle Scholar
Glørstad-Clark, E, Faleide, JI, Lundschien, BA and Nystuen, JP (2010) Triassic seismic sequence stratigraphy and paleogeography of the western Barents Sea area. Marine and Petroleum Geology 27, 1448–75.CrossRefGoogle Scholar
Grogan, P, Nyberg, K, Fotland, B, Myklebust, R, Dahlgren, S and Riis, F (2000) Cretaceous magmatism south and east of Svalbard: evidence from seismic reflection and magnetic data. Polarforschung 68, 25–34.Google Scholar
Grundvåg, SA, Jelby, ME, Śliwińska, KK, Nøhr-Hansen, H, Aadland, T, Sandvik, SE, Tennvassås, I, Engen, T and Olaussen, S (2019) Sedimentology and palynology of the Lower Cretaceous succession of central Spitsbergen: integration of subsurface and outcrop data. Norwegian Journal of Geology 99(2), https://dx.doi.org/10.17850/njg006CrossRefGoogle Scholar
Grundvåg, SA, Marin, D, Kairanov, B, Śliwińska, KK, Nøhr-Hansen, H, Jelby, ME, Escalona, A and Olaussen, S (2017) The Lower Cretaceous succession of the northwestern Barents Shelf: Onshore and offshore correlations. Marine and Petroleum Geology 86, 834–57.CrossRefGoogle Scholar
Grundvåg, SA and Olaussen, S (2017) Sedimentology of the Lower Cretaceous at Kikutodden and Keilhaufjellet, southern Spitsbergen: implications for an onshore–offshore link. Polar Research 36, 1302124.CrossRefGoogle Scholar
Håkansson, E and Pedersen, SAS (2001) The wandel hav strike-slip mobile belt - A mesozoic plate boundary in North Greenland. Bulletin of the Geological Society of Denmark 48, 149–58.Google Scholar
Håkansson, E and Stemmerik, L (1984) Wandel Sea Basin - The North Greenland equivalent to Svalbard and the Barents Shelf. In Petroleum Geology of the North European Margin (ed. Spencer, AM), pp. 97–107. Dordrecht: Springer Netherlands.CrossRefGoogle Scholar
Harland, WBB, Gaskell, BAA, Heaffard, AP, Lind, EKK, Perkins, PJJ, Heafford, AP, Lind, EKK and Perkins, PJJ (1984) Outline of Arctic post-Silurian continental displacements. In Petroleum Geology of the North European Margin (ed. Spencer, AM), pp. 137–48. Dordrecht: Springer Netherlands.CrossRefGoogle Scholar
Harrison, JC, St-Onge, MR, Petrov, OV, Strelnikov, SI, Lopatin, BG, Wilson, FH, Tella, S, Paul, D, Lynds, T, Shokalsky, SP, Hults, CK, Bergman, S, Jepsen, HF and Solli, A (2011) Geological Map of the Arctic. Geological Survey of Canada, Map 2159A, Scale 1:5 000 000, 1–5.CrossRefGoogle Scholar
Helland-Hansen, W and Hampson, GJ (2009) Trajectory analysis: concepts and applications. Basin Research 21, 454–83.CrossRefGoogle Scholar
Helland-Hansen, W and Martinsen, OJ (1996) Shoreline trajectories and sequences; description of variable depositional-dip scenarios. Journal of Sedimentary Research 66, 670–88.Google Scholar
Henderson, RA (2004) A mid-Cretaceous association of shell beds and organic-rich shale; bivalve exploitation of a nutrient-rich, anoxic sea-floor environment. Palaios 19, 156–69.2.0.CO;2>CrossRefGoogle Scholar
Henriksen, E, Bjørnseth, HM, Hals, TK, Heide, T, Kiryukhina, T, Kløvjan, OS, Larssen, GB, Ryseth, AE, Rønning, K, Sollid, K and Stoupakova, A (2011a) Uplift and erosion of the greater Barents Sea: impact on prospectivity and petroleum systems. In Arctic Petroleum Geology (eds Spencer, AM, Embry, AF, Gautier, DL, Stoupakova, AV and Sørensen, K), pp. 271–81. Geological Society of London, Memoir no. 35.Google Scholar
Henriksen, E, Ryseth, AE, Larssen, GB, Heide, T, Ronning, K, Sollid, K and Stoupakova, AV (2011b) Tectonostratigraphy of the greater Barents Sea: implications for petroleum systems. In Arctic Petroleum Geology (eds Spencer, AM, Embry, AF, Gautier, DL, Stoupakova, AV and Sørensen, K), pp. 163–95. Geological Society of London, Memoir no. 35.Google Scholar
Hodgson, DM, Browning, JV, Miller, KG, Hesselbo, SP, Poyatos-Moré, M, Mountain, GS and Proust, J-N (2018) Sedimentology, stratigraphic context, and implications of Miocene intrashelf bottomset deposits, offshore New Jersey. Geosphere 14, 95–114.CrossRefGoogle Scholar
Holbrook, J and Schumm, SA (1999) Geomorphic and sedimentary response of rivers to tectonic deformation: A brief review and critique of a tool for recognizing subtle epeirogenic deformation in modern and ancient settings. Tectonophysics 305(1–3), 287–306.CrossRefGoogle Scholar
Hurum, JH, Roberts, AJ, Dyke, GJ, Grundvåg, SA, Nakrem, HA, Midtkandal, I, Sliwinska, KK and Olaussen, S (2016) Bird or maniraptoran dinosaur? A femur from the Albian strata of Spitsbergen. Palaeontologia Polonica 67, 137–47.Google Scholar
Indrevær, K, Gabrielsen, RH and Faleide, JI (2017) Early Cretaceous synrift uplift and tectonic inversion in the Loppa High area, southwestern Barents Sea, Norwegian shelf. Journal of the Geological Society 174, 242–54.CrossRefGoogle Scholar
Inger, S, Scott, RA and Golionko, BG (1999) Tectonic evolution of the Taimyr Peninsula, northern Russia: implications for Arctic continental assembly. Journal of the Geological Society 156, 1069–72.CrossRefGoogle Scholar
Jackson, HR and Dahl-Jensen, T (2010) Sedimentary and crustal structure from the Ellesmere Island and Greenland continental shelves onto the Lomonosov Ridge, Arctic Ocean. Geophysical Journal International, https://doi.org/10.1111/j.1365-246X.2010.04604.xCrossRefGoogle Scholar
Jones, GED, Hodgson, DM and Flint, SS (2015) Lateral variability in clinoform trajectory, process regime, and sediment dispersal patterns beyond the shelf-edge rollover in exhumed basin margin-scale clinothems. Basin Research 27, 657–80.CrossRefGoogle Scholar
Kairanov, B, Escalona, A, Mordasova, A, Śliwińska, K and Suslova, A (2018) Lower Cretaceous tectonostratigraphic evolution of the northcentral Barents Sea. Journal of Geodynamics 119, 183–98.CrossRefGoogle Scholar
Kayukova, AV and Suslova, AA (2015) A seismostratigraphic analysis of the Lower Cretaceous deposits of the Barents Sea to reveal petroleum perspectives. Moscow University Geology Bulletin 70, 177–82.CrossRefGoogle Scholar
Klausen, TG and Helland-Hansen, W (2018) Methods for restoring and describing ancient clinoform surfaces. Journal of Sedimentary Research 88, 241–59.CrossRefGoogle Scholar
Knudsen, C, Hopper, JR, Bierman, PR, Bjerager, M, Funck, T, Green, PF, Ineson, JR, Japsen, P, Marcussen, C, Sherlock, SC and Thomsen, TB (2018) Samples from the Lomonosov Ridge place new constraints on the geological evolution of the Arctic Ocean. In Circum-Arctic Lithosphere Evolution (eds Pease, V and Coakley, B), pp. 394–418. Geological Society of London, Special Publication no. 460.Google Scholar
Komatsu, T, Ono, M, Naruse, H and Kumagae, T (2008) Upper Cretaceous depositional environments and bivalve assemblages of far-east Asia: the Himenoura Group, Kyushu, Japan. Cretaceous Research 29, 489–508.CrossRefGoogle Scholar
Lebold, JG and Kammer, TW (2006) Gradient analysis of faunal distributions associated with rapid transgression and low accommodation space in a Late Pennsylvanian marine embayment: Biofacies of the Ames Member (Glenshaw Formation, Conemaugh Group) in the northern Appalachian Basin, USA. Palaeogeography, Palaeoclimatology, Palaeoecology 231(3–4), 291–314.CrossRefGoogle Scholar
MacEachern, JA and Bann, KL (2008) The role of ichnology in refining shallow marine facies models. In Recent Advances in Models of Siliciclastic Shallow-Marine Stratigraphy (ed. Hampson, GJ), pp. 73–116. SEPM, Tulsa, Society for Sedimentary Geology.CrossRefGoogle Scholar
Maher, HD (2001) Manifestations of the Cretaceous High Arctic large igneous province in Svalbard. Journal of Geology 109, 91–104.CrossRefGoogle Scholar
Marín, D, Escalona, A, Sliwihska, KK, Nøhr-Hansen, H and Mordasova, A (2017) Sequence stratigraphy and lateral variability of Lower Cretaceous clinoforms in the southwestern Barents Sea. AAPG Bulletin 101, 1487–517.CrossRefGoogle Scholar
Midtkandal, I, Faleide, JI, Dahlberg, ME, Dimitriou, M and Nystuen, JP (2014) The Lower Cretaceous strata in Svalbard and the Barents Sea; basin infill dynamics and palaeobathymetry. In Proceedings of the EGU General Assembly, 27 April–2 May 2014, Vienna, Abstract no. 12638, pp. 2014–12638.Google Scholar
Midtkandal, I, Faleide, TS, Faleide, JI, Planke, S, Anell, I and Nystuen, JP (2019) Nested intrashelf platform clinoforms - evidence of shelf platform growth exemplified by Lower Cretaceous strata in the Barents Sea. Basin Research, published online 22 June 2019, https://doi.org/10.1111/bre.12377CrossRefGoogle Scholar
Midtkandal, I, Holbrook, J, Faleide, JI, Myers, C, Van Yperen, AE, Shephard, GE and Nystuen, JP (2018) Early Cretaceous Arctic palaeotopography as constrained by Barents Sea sediment budget. In AGU Fall Meeting Abstracts, pp. T43I–0525. Washington, DC.Google Scholar
Midtkandal, I and Nystuen, JP (2009) Depositional architecture of a low-gradient ramp shelf in an epicontinental sea: The lower Cretaceous of Svalbard. Basin Research 21, 655–75.CrossRefGoogle Scholar
Midtkandal, I, Nystuen, JP and Nagy, J (2007) Paralic sedimentation on an epicontinental ramp shelf during a full cycle of relative sea-level fluctuation; the Helvetiafjellet Formation in Nordenskiöld land, Spitsbergen. Norsk Geologisk Tidsskrift 87, 343–59.Google Scholar
Midtkandal, I, Nystuen, JP, Nagy, J and Mørk, A (2008) Lower Cretaceous lithostratigraphy across a regional subaerial unconformity in spitsbergen: The Rurikfjellet and Helvetiafjellet Formations. Norsk Geologisk Tidsskrift 88, 287–304.Google Scholar
Midtkandal, I, Svensen, HH, Planke, S, Corfu, F, Polteau, S, Torsvik, TH, Faleide, JI, Grundvåg, SA, Selnes, HH, Kürschner, W and Olaussen, S (2016) The Aptian (Early Cretaceous) oceanic anoxic event (OAE1a) in Svalbard, Barents Sea, and the absolute age of the Barremian-Aptian boundary. Palaeogeography, Palaeoclimatology, Palaeoecology 463, 126–35.CrossRefGoogle Scholar
Minakov, A, Mjelde, R, Faleide, JI, Flueh, ER, Dannowski, A and Keers, H (2012) Mafic intrusions east of Svalbard imaged by active-source seismic tomography. Tectonophysics 518–521, 106–18.CrossRefGoogle Scholar
Minakov, A, Yarushina, V, Faleide, JI, Krupnova, N, Sakoulina, T, Dergunov, N and Glebovsky, V (2018) Dyke emplacement and crustal structure within a continental large igneous province, northern Barents Sea. In Circum-Arctic Lithosphere Evolution (eds Pease, V and Coakley, B), pp. 371–95. Geological Society of London, Special Publication no. 460.Google Scholar
Mørk, A, Dallmann, WK, Dypvik, H, Johannesen, EP, Larssen, GB, Nagy, J, Nøttvedt, A, Olaussen, S, Pchelina, TM and Worsley, D (1999) Mesozoic lithostratigraphy. In Lithostratigraphic Lexicon of Svalbard, Review and Recommendations for Nomenclature Use Review and Recommendations for Nomenclature Use. Upper Palaeozoic to Quaternary Bedrock (ed Dallmann, WK), pp. 127–214. Tromsø: Norwegian Polar Institute.Google Scholar
Mountain, G and Proust, J-N (2010) The New Jersey margin scientific drilling project (IODP Expedition 313): Untangling the record of global and local sea-level changes. Scientific Drilling 10, 26–34, https://doi.org/10.2204/iodp.sd.10.03.2010CrossRefGoogle Scholar
Mutrux, J, Maher, H, Shuster, R and Hays, T (2008) Iron ooid beds of the Carolinefjellet Formation, Spitsbergen, Norway. Polar Research 27, 28–43.CrossRefGoogle Scholar
Nagy, J (1970) Ammonite faunas and stratigraphy of Lower Cretaceous (Albian) rocks in southern Spitsbergen. Norsk Polarinstitutt Skrifter 152, 1–58.Google Scholar
Nemec, W (1992) Depositional controls on plant growth and peat accumulation in a braidplain delta environment: Helvetiafjellet Formation (Barremian-Aptian), Svalbard. In Controls on the Distribution and Quality of Cretaceous Coals (eds PJ McCabe and JT Parrish), pp. 209–26. Geological Society of America, Special Paper no. 267.CrossRefGoogle Scholar
Norwegian Petroleum Directorate (NPD) (2017) Geologisk vurdering av petroleumsressursene i østlige deler av Barentshavet nord 2017, 40 p. Report by Norwegian Petroleum Directorate, Stavanger, Norway.Google Scholar
Nøttvedt, A, Cecchi, M, Gjelberg, JG, Kristensen, SE and Lønøy, A (1993) Svalbard–Barents Sea correlation: a short review. In Arctic Geology and Petroleum Potential: Proceedings of the Norwegian Petroleum Society Conference (eds Vorren, TO, Bergsager, E, Dahl-Stamnes, ØA, Holter, E, Johansen, B, Lie, E and Lund, TB), pp. 363–75. Tromsø, Norway: Elsevier.Google Scholar
Nøttvedt, A and Kreisa, RD (1987) Model for the combined-flow origin of hummocky cross-stratification. Geology 15, 357.2.0.CO;2>CrossRefGoogle Scholar
Olaussen, S, Larssen, GB, Helland-Hansen, W, Johannessen, EP, Nøttvedt, A, Riis, F, Rismyhr, B, Smelror, M and Worsley, D (2019) Mesozoic strata of Kong Karls Land, Svalbard, Norway; a link to the northern Barents Sea basins and platforms. Norwegian Journal of Geology 98(4), https://dx.doi.org/10.17850/njg.98-4-06CrossRefGoogle Scholar
Parker, JR (1967) The Jurassic and Cretaceous Sequence in Spitsbergen. Geological Magazine 104, 487–505.CrossRefGoogle Scholar
Patruno, S, Hampson, GJ and Jackson, CAL (2015) Quantitative characterisation of deltaic and subaqueous clinoforms. Earth-Science Reviews 142, 79–119.CrossRefGoogle Scholar
Pease, V, Drachev, S, Stephenson, R and Zhang, X (2014) Arctic lithosphere - A review. Tectonophysics 628, 1–25.CrossRefGoogle Scholar
Piepjohn, K, von Gosen, W and Tessensohn, F (2016) The Eurekan deformation in the Arctic: an outline. Journal of the Geological Society 173, 1007–24.CrossRefGoogle Scholar
Polteau, S, Hendriks, BWH, Planke, S, Ganerød, M, Corfu, F, Faleide, JI, Midtkandal, I, Svensen, HS and Myklebust, R (2015a) The Early Cretaceous Barents Sea Sill Complex: distribution, 40Ar/39Ar geochronology, and implications for carbon gas formation. Palaeogeography, Palaeoclimatology, Palaeoecology 441, 83–95.CrossRefGoogle Scholar
Polteau, S, Mazzini, A and Planke, S (2015b) BSS14 – Barents Sea Sampling Project 2014 – Barents SE Area. Commercial Report, Volcanic Basin Petroleum Research, Oslo. VBPR/TGS report, 112 p.Google Scholar
Rasmussen, ES, Dybkjær, K and Piasecki, S (2010) Lithostratigraphy of the Upper Oligocene–Miocene succession of Denmark. Geological Survey of Denmark and Greenland Bulletin 22, 92.Google Scholar
Rivera, J, Karabanov, EB, Williams, DF, Buchinskyi, V and Kuzmin, M (2006) Lena River discharge events in sediments of Laptev Sea, Russian Arctic. Estuarine, Coastal and Shelf Science 66, 185–96.CrossRefGoogle Scholar
Schumm, SA (1993) River response to baselevel change: implications for sequence stratigraphy. Journal of Geology 101, 279–94.CrossRefGoogle Scholar
Senger, K, Tveranger, J, Ogata, K, Braathen, A and Planke, S (2014) Late Mesozoic magmatism in Svalbard: a review. Earth-Science Reviews 139, 123–44.CrossRefGoogle Scholar
Serck, CS, Faleide, JI, Braathen, A, Kjølhamar, B and Escalona, A (2017) Jurassic to Early Cretaceous basin configuration(s) in the Fingerdjupet Subbasin, SW Barents Sea. Marine and Petroleum Geology 86, 874–91.CrossRefGoogle Scholar
Shephard, GE, Flament, N, Williams, S, Seton, M, Gurnis, M and Müller, RD (2014) Circum-Arctic mantle structure and long-wavelength topography since the Jurassic. Journal of Geophysical Research B: Solid Earth 119, 7889–908.Google Scholar
Shephard, GE, Müller, RD and Seton, M (2013) The tectonic evolution of the Arctic since Pangea breakup: Integrating constraints from surface geology and geophysics with mantle structure. Earth-Science Reviews 124, 148–83.Google Scholar
Shipilov, EV (2008) Generations of spreading basins and stages of breakdown of Wegener’s pangea in the geodynamic evolution of the Arctic Ocean. Geotectonics 42, 105–24.CrossRefGoogle Scholar
Sigmond, EMO (2002) Geologisk kart over land- og havområder i Nord-Europa, målestokk 1:4 mil. Geological Survey of Norway, Trondheim, Norway.Google Scholar
Smelror, M, Larssen, GB, Olaussen, S, Rømuld, A and Williams, R (2019) Late Triassic to Early Cretaceous palynostratigraphy of Kong Karls Land, Svalbard, Arctic Norway, with correlations to Franz Josef Land, Arctic Russia. Norwegian Journal of Geology 98, https://dx.doi.org/10.17850/njg004CrossRefGoogle Scholar
Smelror, M, Mørk, A, Monteil, E, Rutledge, D and Leereveld, H (1998) The Klippfisk formation - a new lithostratigraphic unit of Lower Cretaceous platform carbonates on the Western Barents Shelf. Polar Research 17, 181–202.Google Scholar
Smelror, M, Mørk, A, Mørk, MB, Weiss, HM and Løseth, H (2001) Middle Jurassic-Lower Cretaceous transgressive-regressive sequences and facies distribution off Northern Nordland and Troms, Norway. Norwegian Petroleum Society Special Publications 10, 211–32.CrossRefGoogle Scholar
Smelror, M, Petrov, OV, Larssen, GB and Werner, S (2009) Geological History of the Barents Sea. Geological Survey of Norway, Trondheim, 135 p.Google Scholar
Smith, DG, Harland, WB, Hughes, NF and Pickton, CAG (1976) The geology of Kong Karls Land, Svalbard. Geological Magazine 113, 193–304.CrossRefGoogle Scholar
Solheim, A, Gustavsen, F, Musatov, E and Dypvik, H (1998) The shallow subsurface geology of the northeastern Barents Sea. In Geological Aspects of Franz Josef Land and the Northernmost Barents Sea (eds Solheim, A, Musatov, E and Heinz, N), pp. 24–49. Norsk Polarinstututt, Tromsø, Meddelelser 151.Google Scholar
Sømme, TO, Doré, AG, Lundin, ER and Tørudbakken, BO (2018) Triassic–Paleogene paleogeography of the Arctic: Implications for sediment routing and basin fill. AAPG Bulletin 102, 2481–517.CrossRefGoogle Scholar
Suslova, AA (2013) Seismostratigraphic complex of Jurassic deposits, Barents Sea shelf. Moscow University Geology Bulletin 68, 207–09.CrossRefGoogle Scholar
Svendsen, JI, Gataullin, V, Mangerud, J and Polyak, L (2004) The glacial history of the Barents and Kara Sea region. In Quaternary Glaciations – Extent and Chronology (eds Ehlers, J, Gibbard, PL and Hughes, PD), pp. 369–78. Elsevier, Developments in Quaternary Sciences vol. 15.CrossRefGoogle Scholar
Torsvik, TH and Andersen, TB (2002) The Taimyr fold belt, Arctic Siberia: timing of prefold remagnetisation and regional tectonics. Tectonophysics 352, 335–48.CrossRefGoogle Scholar
Torsvik, TH and Cocks, LRM (2016) Cretaceous. In Earth History and Palaeogeography (eds Cocks, R and Torsvik, TH), pp. 219–39. Cambridge: Cambridge University Press.Google Scholar
Torsvik, TH, Van der Voo, R, Preeden, U, Mac Niocaill, C, Steinberger, B, Doubrovine, PV, van Hinsbergen, DJJ, Domeier, M, Gaina, C, Tohver, E, Meert, JG, McCausland, PJA and Cocks, LRM (2012) Phanerozoic polar wander, palaeogeography and dynamics. Earth-Science Reviews 114, 325–68.CrossRefGoogle Scholar
Vickers, ML, Price, GD, Jerrett, RM and Watkinson, M (2016) Stratigraphic and geochemical expression of Barremian–Aptian global climate change in Arctic Svalbard. Geosphere 12, GES01344.1.CrossRefGoogle Scholar
Vorren, TO, Hald, M and Lebesbye, E (1988) Late Cenozoic environments in the Barents Sea. Paleoceanography 3, 601–12.CrossRefGoogle Scholar
Wood, RJ, Edrich, SP and Hutchison, I (1989) Influence of North Atlantic tectonics on the large- scale uplift of the Stappen High and the Loppa High, western Barents Shelf. In Extensional Tectonics and Stratigraphy of the North Atlantic Margins (eds Tankard, AJ and Balkwill, HR), pp. 559–566. AAPG, Tulsa, Memoir no. 46.Google Scholar
Worsley, D (2008) The post-Caledonian development of Svalbard and the western Barents Sea. Polar Research 27, 298–317.CrossRefGoogle Scholar
Worsley, D, Johansen, R and Kristensen, SE (1988) The Mesozoic and Cenozoic succession of Tromsøflaket. Norwegian Petroleum Directorate Bulletin 4, 42–65.Google Scholar
Zhang, X, Pease, V, Skogseid, J and Wohlgemuth-Ueberwasser, C (2015) Reconstruction of tectonic events on the northern Eurasia margin of the Arctic, from U-Pb detrital zircon provenance investigations of late Paleozoic to Mesozoic sandstones in southern Taimyr Peninsula. Geological Society of America Bulletin 128, B31241.1.CrossRefGoogle Scholar
Ziegler, PA (1988) Late Jurassic-Early Cretaceous Central Atlantic sea-floor spreading, closure of Neo-Tethys, and opening of Canada Basin. In Evolution of the Arctic-North Atlantic and the Western Tethys (ed. Ziegler, PA), pp. 63–82. AAPG, Tulsa, Memoir no. 43.Google Scholar