Late Permian to Triassic basin infill history and palaeogeography of the Mid-Norwegian shelf—East Greenland region
References (57)
- et al.
Sedimentary environments offshore Norway—an overview
Alternating aeolian, sabkha and shallow-lake deposits from the middle Triassic Gipsdalen Formation, Scoresby Lands, East Greenland
Paleogeogr., Paleoclimat., Paleoecol.
(1978)- et al.
A late Triassic lake system in East-Greenland: facies, depositional cycles and palaeoclimate
Paleogeogr., Paleoclimat., Palcoecol.
(1998) - et al.
Structure of the Møre Basin, mid-Norway continental margin
Tectonophysics
(1995) - et al.
Upper Permian lowstand fans of the Bredehorn Member, Schuchert Dal Formation, East Greenland
Incised submarine canyons governing new evidence of Early Triassic rifting in East Greenland
Palaeogeogr., Palcoclimat., Palaeoecol.
(2000)Sedimentary facies and depositional environment of early Mesozoic Newark Supergroup basins, castern North America
Palaeogeogr., Paleoclimat., Palaeoecol.
(1991)Late Paleozoic evolution of the North Atlantic margin of Pangea
Palaeogeogr., Paleoclimat., Palaeoecol.
(2000)- et al.
Depositional history and petroleum geology of the Carboniferous to Cretaceous sediments in the northern part of East Greenland
- et al.
Late Palaeozoic-Mesozoic evolution of central East Greenland
Erosional unconformity at the base of marine Lower Triassic at Wegener Ø, central East Greenland
Grønl. Geol. Under., Rapp.
Structural elements of the Norwegian continental shelf, Part II: The Norwegian Sea Region
NPD, Bull.
Tectonics and basin evolution of the Norwegian shelf between 62'N and 72'N
Norsk Geol. Tidsskr.
The prospectivity of the Vøring and Møre Basins on the Norwegian Sea continental margin
Upper Permian as a new play model on the mid-Norwegian continental shelf; Investigated by shallow stratigraphic drilling
AAPG Bull.
Structure and development of the mid-Norway Continental Margin
Triassic lithostratigraphhy of East Greenland between Scoresby Sund and Kejser Franz Josephs Fjord
Grønl. Geol. Unders., Bull.
Triassic rift sedimentation and palaeogeography of central East Greenland
Grønl. Geol. Unders., Bull.
Synoptic palaeogeography of the Northeast Atlantic Seaway: late Permian to Cretaceous
Tectonic and climate control of Triassic sedimentation in the Beryl Basin, northern North Sea
J. Geol. Soc., London
Tectono-sedimentary evolution of active extensional basins
Basin Res.
Fission-track and K-Ar dating of tectonic activity in a transect across the Møre-Trøndelag Fault Zone, central Norway
Norsk Geol. Tidsskr.
Triassic sequence stratigraphic framework of western European Basins. Mesozoic and Cenozoic Sequence Stratigraphy of European Basins
SEPM Spec. Publ.
A Phanerozoic Time Scale
Episodes
Basin development and hydrocarbon occurrence offshore Mid-Norway
The Triassic offshore Norway north of 62°N
Potential reservoir and source rocks in relation to Upper Triassic to Middle Jurassic sequence stratigraphy, Atlantic margin basins of the British Isles
Cited by (62)
The influence of orogenic collision inheritance on rifted margin architecture: Insights from comparing numerical experiments to the Mid-Norwegian margin
2022, TectonophysicsCitation Excerpt :A first phase of extensional rifting is imposed at an ultra-slow opening rate of 0.1 cm/yr, over 40 Myrs, from 300 to 260 Ma, corresponding to Permian times. This phase aims at representing the tectonic stage responsible for the formation of basins identified in the proximal settings of the Mid-Norwegian margins, according to the results of various authors (e.g., Muller et al., 2005; Faleide et al., 2010; Hansen et al., 2012). For instance, the proximal Vøring domain is usually interpreted as a platform -type environment floored by a sub-basin system filled by Permian and Early Triassic sediments (Blystad et al., 1995).
Late Triassic paleowinds from lacustrine wave ripple marks in the Fleming Fjord Group, central East Greenland
2022, Palaeogeography, Palaeoclimatology, PalaeoecologyThe proximal domain of the Mid-Norwegian rifted margin: The Trøndelag Platform revisited
2020, TectonophysicsCitation Excerpt :In the current contribution, the stratigraphy has been mapped based on three different sets of constraints: 1. The horizons from the seafloor down to the ‘Base Carnian / Late Ladinian evaporite marker’ are constrained based on well calibrations (Muller et al., 2005); 2. The underlying ‘intra Late Permian’ horizon is interpreted based on Bugge et al. (2002) and Muller et al. (2005) results and publications; 3.
Norwegian Sea area Permo-Triassic organic-carbon-rich deposits from seismic
2020, Marine and Petroleum Geology