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Trondelag Platform

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Series: Geological Society, London, Petroleum Geology Conference Series
Published: 01 January 2005
DOI: 10.1144/0061147
EISBN: 9781862394124
.... Smaller turbidite systems developed along the Norwegian margin, which were sourced from the east from smaller drainage areas, and partially across broad shelves, such as the Trøndelag Platform. Both in the Cretaceous and Palaeogene, the sandiest systems are found only to the south and the north...
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Series: Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.167.01.13
EISBN: 9781862394155
... Abstract The Norwegian Sea continental margin is dominated by two major basins with a very thick Cretaceous basin fill: the Vøring and Møre Basins. The basins are flanked by the uplifted mainland and the Cretaceous Trøndelag Platform to the east and by the Møre and Vøring Marginal Highs capped...
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Journal Article
Journal: GSA Bulletin
Published: 01 May 2010
GSA Bulletin (2010) 122 (5-6): 884–896.
...Peter A. Hochuli; Jorunn Os Vigran; Elke Hermann; Hugo Bucher Abstract Here, we present the palynological record from two shallow core holes (6611/09-U-01 and -02) from the Trøndelag Platform offshore mid-Norway consisting of 750 m of Upper Permian and Lower Triassic sediments. The relatively...
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Series: Geological Society, London, Petroleum Geology Conference Series
Published: 01 January 2010
DOI: 10.1144/0070885
EISBN: 9781862394131
... the base of the sedimentary strata. Sedimentary thickness is larger than 14 km on the mid-Norwegian margin and the Barents Sea, but varies strongly along the different segments of the margin. In the northeastern North Sea, the Danish–Norwegian Basin, and over the Trøndelag Platform the top basement does...
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Journal Article
Published: 01 October 2004
Petroleum Geoscience (2004) 10 (4): 353–365.
...-flow measurements conducted in this survey was 58.5 mW m −2 , with a standard error of ±4.40 mW m −2 . The mean heat flow from IKU well data for the Trøndelag Platform is 56.2±6.65 mW m −2 . Shorter wavelength heat-flow variations appear to be controlled structurally and can be explained...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 2002
AAPG Bulletin (2002) 86 (1): 107–127.
... mudstones. Reworked fragments of reef-building organisms in Upper Permian turbidites and Upper Permian carbonates encountered in an exploration well on the Nordland Ridge indicate that carbonate deposition and reef building occurred on structural highs on the Trondelag Platform. The observations from...
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Journal Article
Journal: GSA Bulletin
Published: 01 December 1999
GSA Bulletin (1999) 111 (12): 1792–1807.
... on the Trøndelag platform. This event was followed by a period of margin subsidence and modest sedimentation until late Pliocene time. Although Miocene and early Pliocene biosiliceous hemipelagic sediments dominate on the outer margin, the influx of ice-rafted detritus records the climatic deterioration...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1998
AAPG Bulletin (1998) 82 (2): 274–290.
... on the basis of a combination of heavy mineral parameters. Sandstone type K1 occurs on the Trøndelag Platform, Halten Terrace, and Nordland Ridge, but does not appear to be present in the deeper water Vøring Basin. Sandstone type K1 was ultimately derived from the Scandinavian landmass with detritus sourced...
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Magnetic anomaly map of Norway and adjacent ocean areas (based on  Olesen  ...
Published: 01 September 2002
Platform–Vøring Basin. The continent–ocean boundary (COB) is shown as a bold black line. Crustal-scale cross-section through mid-Norway, the Trøndelag Platform and the Vøring Basin into the oceanic crust is after Mosar (2000) . The main structural features of the Mid-Norway offshore region are indicated
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Regional map of western Norwegian seaboard, showing location of three-dimen...
Published: 01 April 2010
Figure 1. Regional map of western Norwegian seaboard, showing location of three-dimensional seismic survey in Møre Basin. JMFZ—Jan Mayen Fracture Zone, TP—Trondelag Platform, HT—Halten Terrace.
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Regional cross-section of the Vøring margin from the Vøring Marginal High t...
Published: 01 March 2003
Fig. 3.  Regional cross-section of the Vøring margin from the Vøring Marginal High to the Trøndelag Platform. IF, inner flows; LF, landward flows; SDR, seaward-dipping reflectors. Location is shown in Figure 1 .
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Offshore Norway base map with location of well 6505/10–1 in the Vøring Basi...
Published: 01 February 2011
Fig. 1 Offshore Norway base map with location of well 6505/10–1 in the Vøring Basin (VB), HT, Halten Terrace; TP, Trøndelag Platform; MMH, Møre Marginal High; VMH, Vøring Marginal High.
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Chronostratigraphic well correlations: ( a ) across the Halten Terrace; ( b...
Published: 01 December 2001
Fig. 5 Chronostratigraphic well correlations: ( a ) across the Halten Terrace; ( b ) along the Halten Terrace and Trøndelag Platform; and ( c ) along the Halten and Dønna terraces. For location of wells see Figure 1 . Time-scale in Figure 4 .
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Paleogeographic position and location of the discussed sections, e.g., core...
Published: 01 May 2010
Figure 1. Paleogeographic position and location of the discussed sections, e.g., cores 6611/09-U-01 and -02 on the Trøndelag Platform, offshore mid-Norway, and the section from East Greenland (Jameson Land). The paleogeography is based on the compilation of Smith et al. (1994) .
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Results of the Møre Margin modelling and comparison with the Vøring Margin....
Published: 01 December 2005
Fig. 5.  Results of the Møre Margin modelling and comparison with the Vøring Margin. CL, coastline; UC, upper crust; LC, continental lower crust; OCB, ocean–continent boundary (origin of the models). The gap in the Møre profiles simulates the absent Trøndelag Platform structure.
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Heat-flow histories derived from different  ß  factors. Pre-rifting crustal...
Published: 01 October 2004
Fig. 7 Heat-flow histories derived from different ß factors. Pre-rifting crustal conditions calibrated against Trøndelag Platform. One-dimensional finite element model. Initial lithospheric thickness 100 km, initial crustal thickness 30 km, duration of rifting 30 (60) Ma. Temperature at base
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Schematic reconstruction of the Late Permian-Early Triassic basin between N...
Published: 01 January 2002
Figure 15 Schematic reconstruction of the Late Permian-Early Triassic basin between Norway and Greenland. All the cored units on the Norwegian side can be recognized in East Greenland. In the Late Permian, the Trøndelag Platform was probably characterized by local basins that had deposition
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( a ) Map of North Atlantic passive margin with continent–ocean boundary (C...
Published: 01 January 2010
Fig. 1. ( a ) Map of North Atlantic passive margin with continent–ocean boundary (COB) after Müller et al . (2008 ). Red line marks present-day spreading ridge. TP, Trøndelag Platform. ( b ) Overview map of Scandinavia showing large-scale topography and bathymetry (from Dehls et al . 2000
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Chronostratigraphic and lithological succession of the sections penetrated ...
Published: 01 May 2010
Figure 3. Chronostratigraphic and lithological succession of the sections penetrated by the shallow cores 6611/09-U-01 and -02 on the Trøndelag Platform, offshore mid-Norway (after Bugge et al., 2002 ) and the original sample depth in the respective cores (see arrows). Hygrophyte/xerophyte
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(A) Main structural elements of the continental shelf and margin off mid-No...
Published: 01 August 2005
Figure 2 (A) Main structural elements of the continental shelf and margin off mid-Norway and location of regional profile in (B). MB = Møre Basin; VB = Vøring Basin; HT = Halten Terrace; TP = Trøndelag Platform (A and B modified from Blystad et al., 1995 ). (C, D) Seismic cross section across