Triassic rocks in Svalbard, the Arctic Soviet islands and the Barents Shelf: bearing on their correlations

Mørk, Atle; Vigran, Jorunn Os; Korchinskaya, M. V.; Pchelina, Tatyana M; Fefilova, L.A.; Vavilov, M.N.; Weitschat, Wolfgang

doi:10.1016/b978-0-444-88943-0.50033-2

Cited by 31 publications

(56 citation statements)

References 23 publications

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“…Several publications have dealt with regional aspects of the Triassic in the Barents Sea (Berglund et al, 1986;Embry and Mørk, 2006;Jacobsen and van Veen, 1984;Johansen et al, 1993;Mørk et al, , 1982Mørk et al, , 1993Mørk and Elvebakk, 1999;Skjold et al, 1998;, but this study includes more data on a regional scale compared to the other studies, particularly in the northern part of the study area.…”

Section: Introductionmentioning

confidence: 90%

“…Various authors have proposed that global or circum-Arctic sequence boundaries occur within the Triassic succession (Egrov and Mørk, 2000;Embry and Mørk, 2006;Embry, 1997;Mørk, 1994;Mørk et al, 1989Mørk et al, , 1993Mørk and Worsley, 2006;Skjold et al, 1998;. Based on publications from the Arctic, it is clear that the sequence development in the Triassic has similarities in the different basins (i.e.…”

Section: Sequence Stratigraphic Developmentmentioning

confidence: 96%

“…However, the various sequence stratigraphic schemes are based on assorted data-sets and study methods, making it challenging to correlate between the different basins. We have divided the Triassic into five second-order sequences, a subdivision that partly differs from similar sequence stratigraphic studies in the Barents Sea, Sverdrup Basin and on main Svalbard Archipelago (Embry and Mørk, 2006;Embry, 1997;Mørk, 1994;Mørk et al, 1989Mørk et al, , 1993Skjold et al, 1998;. The sequences are approximately of the same order and potentially also regional extent, but they differ in study methods, sequence stratigraphic concepts and lack of highresolution biostratigraphic control.…”

Section: Sequence Stratigraphic Developmentmentioning

confidence: 97%

“…However, the sedimentary succession was influenced by northwards drift and climatic variation, controlling the types of sediments in this area (Jacobsen and van Veen, 1984;Mørk et al, 1993;P celina and Kor cinskaja, 2008). The main Svalbard Archipelago moved from about 40e50 N during the Triassic and deposition occurred in an arid to humid climate with periodic restricted circulation (Steel and Worsley, 1984).…”

Section: Geological Settingmentioning

confidence: 97%

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Triassic seismic sequence stratigraphy and paleogeography of the western Barents Sea area

Glørstad-Clark

Faleide

Lundschien³

et al. 2010

Marine and Petroleum Geology

180

255

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Section: Introductionmentioning

confidence: 90%

Section: Sequence Stratigraphic Developmentmentioning

confidence: 96%

Section: Sequence Stratigraphic Developmentmentioning

confidence: 97%

Section: Geological Settingmentioning

confidence: 97%

See 2 more Smart Citations

Triassic seismic sequence stratigraphy and paleogeography of the western Barents Sea area

Glørstad-Clark

Faleide

Lundschien³

et al. 2010

Marine and Petroleum Geology

180

255

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“…A marine seaway between East Greenland and Norway was connected to the seas covering Svalbard, the Sverdrup Basin and NW Siberia in the Early Triassic (Mørk et al 1992;Seidler et al 2004;Müller et al 2005;Bjerager et al 2006).…”

Section: Central East Greenland Marginmentioning

confidence: 99%

An overview of the Upper Palaeozoic–Mesozoic stratigraphy of the NE Atlantic region

Stoker

Stewart

Shannon

et al. 2016

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This study describes the distribution and stratigraphic range of the Upper PalaeozoicMesozoic succession in the NE Atlantic region, and is correlated between conjugate margins and along the axis of the NE Atlantic rift system. The stratigraphic framework has yielded important new constraints on the timing and nature of sedimentary basin development in the NE Atlantic, with implications for rifting and the break-up of the Pangaean supercontinent. From a regional perspective, the Permian-Triassic succession records a northwards transition from an arid interior to a passively subsiding, mixed carbonate -siliciclastic shelf margin. A Late Permian-earliest Triassic rift pulse has regional expression in the stratigraphic record. A fragmentary paralic to shallowmarine Lower Jurassic succession reflects Early Jurassic thermal subsidence and mild extensional tectonism; this was interrupted by widespread Mid-Jurassic uplift and erosion, and followed by an intense phase of Late Jurassic rifting in some (but not all) parts of the NE Atlantic region. The Cretaceous succession is dominated by thick basinal-marine deposits, which accumulated within and along a broad zone of extension and subsidence between Rockall and NE Greenland. There is no evidence for a substantive and continuous rift system along the proto-NE Atlantic until the Late Cretaceous.Gold Open Access: This article is published under the terms of the CC-BY 3.0 license.

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Triassic platform-margin deltas in the western Barents Sea

Glørstad-Clark

Birkeland²,

Nystuen

et al. 2011

Marine and Petroleum Geology

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Triassic rocks in Svalbard, the Arctic Soviet islands and the Barents Shelf: bearing on their correlations

Cited by 31 publications

References 23 publications

Triassic seismic sequence stratigraphy and paleogeography of the western Barents Sea area

Triassic seismic sequence stratigraphy and paleogeography of the western Barents Sea area

An overview of the Upper Palaeozoic–Mesozoic stratigraphy of the NE Atlantic region

Triassic platform-margin deltas in the western Barents Sea

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