Search Results - "Surlyk, Finn"
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Jurassic stratigraphy of East Greenland
Published in GEUS Bulletin (01-01-2021)“…The East Greenland Rift Basin comprises a series of Jurassic subbasins with different crustal configurations, and somewhat different tectonic histories and…”
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Sea-level change and facies development across potential Triassic-Jurassic boundary horizons, SW Britain
Published in Journal of the Geological Society (01-05-2004)“…The Late Triassic to Early Jurassic aged succession of SW Britain (the Penarth and lower Lias Groups) comprises mudstone, sandstone and limestone strata…”
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Upper Cretaceous chalk facies and depositional history recorded in the Mona-1 core, Mona Ridge, Danish North Sea
Published in Geological Survey of Denmark and Greenland bulletin (2011)“…The 331 m long core from the Mona-1 well in the Danish North Sea spans almost the entire Upper Cretaceous Chalk Group but only about 10% of Late Cretaceous…”
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Coarse‐grained, marine, sub‐wave base, high‐angle clinoform sets: A little‐known outcrop facies illustrated by Jurassic examples from East Greenland
Published in Basin research (01-08-2023)“…Outcrops of coarse‐grained, high‐angle clinoform sets are mainly thought to represent Gilbert‐type deltas. Superficially similar clinoform sets may, however,…”
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Long runout distance of a block breccia density flow along a half-graben axis: latest Jurassic rift climax in East Greenland
Published in Journal of the Geological Society (03-03-2023)“…A basinally isolated breccia–pebbly sandstone couplet occurs in the axial part of the latest Jurassic rift-climax half-graben in Wollaston Forland, East…”
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Long run-out distance of a block breccia density flow along a halfgraben axis; latest Jurassic rift climax in East Greenland
Published in Journal of the Geological Society (16-11-2022)“…A basinally-isolated breccia-pebbly sandstone couplet occurs in the axial part of the latest Jurassic rift-climax halfgraben in Wollaston Forland, East…”
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Marine macrofossil communities in the uppermost Maastrichtian chalk of Stevns Klint, Denmark
Published in Palaeogeography, palaeoclimatology, palaeoecology (01-04-2014)“…Three successive marine habitats and their benthic macrofossil communities have been recognised and assessed in the uppermost Maastrichtian chalk of Stevns…”
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Uplift, deflation and marine onlap of a Jurassic rift dome, illustrated by a backstepping Middle–Upper Jurassic shelf‐to‐slope succession, Geographical Society Ø, East Greenland
Published in Terra nova (Oxford, England) (01-12-2023)“…Abstract “Doming–rifting–spreading” constitute the main phases of classical plate tectonics. The Middle–Upper Jurassic succession of East Greenland is…”
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The influence of depositional processes on the porosity of chalk
Published in Journal of the Geological Society (01-05-2012)“…Chalk constitutes challenging low-permeability reservoirs with porosity variations attributable to complex interactions between numerous processes. The…”
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Adaptive morphologies of the brachiopod fauna from Danian coral mounds at Faxe, Denmark
Published in Palaeogeography, palaeoclimatology, palaeoecology (15-11-2019)“…Only few of the brachiopod species that lived in the Late Cretaceous Chalk Sea of northern Europe survived the mass extinction at the Cretaceous–Paleogene…”
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A Giant Sand Injection Complex: The Upper Jurassic Hareelv Formation of East Greenland
Published in Geologia Croatica (01-06-2003)“…A major intrusive sandstone complex of Late Jurassic age is spectacularlyexposed in Jameson land, East Greenland. It is probably thelargest in the World, and…”
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First record of the cosmopolitan brachiopod Praelacazella wetherelli from the lower Maastrichtian of Western Australia
Published in Cretaceous research (01-08-2024)“…We describe the thecideid brachiopod Praelacazella wetherelli (Morris, 1851) from the lower Maastrichtian Korojon Formation in the Carnarvon Basin, Western…”
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Adaptive brachiopod morphologies in four key environments of the Late Cretaceous–Danian Chalk Sea of northern Europe: A comparative study
Published in Cretaceous research (01-03-2020)“…Rich brachiopod faunas are known from the four main, but highly different, palaeoenvironments in the Late Cretaceous–Danian Chalk Sea of northern Europe:…”
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Late Cretaceous (late Campanian–Maastrichtian) sea-surface temperature record of the Boreal Chalk Sea
Published in Climate of the past (24-02-2016)“…The last 8 Myr of the Cretaceous greenhouse interval were characterized by a progressive global cooling with superimposed cool/warm fluctuations. The…”
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Morphological adaptations of the brachiopods from a Late Cretaceous rocky shore, Ivö Klack, southern Sweden
Published in Palaeogeography, palaeoclimatology, palaeoecology (15-01-2019)“…In 1965 D.V. Ager highlighted the concept of morphological adaptations of Mesozoic brachiopods to different environments. Rocky shores were only indirectly…”
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Crestal unconformities on an exposed Jurassic tilted fault block, Wollaston Forland, East Greenland as an analogue for buried hydrocarbon traps
Published in Marine and petroleum geology (01-06-2013)“…The stratigraphy of successions exposed in footwall crests of tilted fault blocks is commonly highly complex. Crestal stratigraphy and structure are…”
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Upper Campanian–Maastrichtian holostratigraphy of the eastern Danish Basin
Published in Cretaceous research (01-11-2013)“…One of the most expanded upper Campanian–Maastrichtian successions worldwide has been cored in a series of boreholes in eastern Denmark. A high-resolution…”
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Facies and ichnology of an Upper Cretaceous chalk contourite drift complex, eastern Denmark, and the validity of contourite facies models
Published in Journal of the Geological Society (01-07-2012)“…The Upper Cretaceous chalk of the Danish Basin has been interpreted as a major contourite complex on the basis of high-resolution seismic data. The sea floor…”
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Depositional processes and stratigraphic architecture within a coarse-grained rift-margin turbidite system: The Wollaston Forland Group, east Greenland
Published in Marine and petroleum geology (01-09-2016)“…The Wollaston Forland Basin, NE Greenland, is a half-graben with a Middle Jurassic to Lower Cretaceous basin-fill. In this outcrop study we investigate the…”
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