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Relevant bibliographies by topics / Cromer Knoll

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Academic literature on the topic 'Cromer Knoll'

Author: Grafiati

Published: 4 June 2021

Last updated: 15 February 2022

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Journal articles on the topic "Cromer Knoll"

1

Moscardelli, Lorena, Sarika K. Ramnarine, Lesli Wood, and Dallas B. Dunlap. "Seismic geomorphological analysis and hydrocarbon potential of the Lower Cretaceous Cromer Knoll Group, Heidrun field, Norway." AAPG Bulletin 97, no. 8 (2013): 1227–48. http://dx.doi.org/10.1306/02081312155.

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2

Japsen, Peter, Peter Britze, and Claus Andersen. "Upper Jurassic – Lower Cretaceous of the Danish Central Graben: structural framework and nomenclature." Geological Survey of Denmark and Greenland (GEUS) Bulletin 1 (October 28, 2003): 231–46. http://dx.doi.org/10.34194/geusb.v1.4653.

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The Danish Central Graben is part of the mainly Late Jurassic complex of grabens in the central and southern North Sea which form the Central Graben. The tectonic elements of the Danish Central Graben in the Late Jurassic are outlined and compared to those in the Early Cretaceous based on reduced versions of published maps (1:200 000), compiled on the basis of all 1994 public domain seismic and well data. The Tail End Graben, a half-graben which stretches for about 90 km along the East North Sea High, is the dominant Late Jurassic structural feature. The Rosa Basin (new name) is a narrow, nort

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3

van Buchem, F. S. P., F. W. H. Smit, G. J. A. Buijs, B. Trudgill, and P. H. Larsen. "Tectonostratigraphic framework and depositional history of the Cretaceous–Danian succession of the Danish Central Graben (North Sea) – new light on a mature area." Geological Society, London, Petroleum Geology Conference series 8, no. 1 (2017): 9–46. http://dx.doi.org/10.1144/pgc8.24.

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AbstractAn integrated tectonic and sequence stratigraphic analysis of the Cretaceous and Danian of the Danish Central Graben has led to significant new insights critical for our understanding of the chalk facies as a unique cool-water carbonate system, as well as for the evaluation of its potential remaining economic significance.A major regional unconformity in the middle of the Upper Cretaceous chalk has been dated as being of early Campanian age. It separates two distinctly different basin types: a thermal contraction early post-rift basin (Valanginian–Santonian), which was succeeded by an

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4

Schovsbo, Niels Hemmingsen, Louise Ponsaing, Anders Mathiesen, et al. "Regional hydrocarbon potential and thermal reconstruction of the Lower Jurassic to lowermost Cretaceous source rocks in the Danish Central Graben." Bulletin of the Geological Society of Denmark 68 (September 14, 2020): 195–230. http://dx.doi.org/10.37570/bgsd-2020-68-09.

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The Danish part of the Central Graben (DCG) is one of the petroliferous basins in the offshore region of north-western Europe. The source rock quality and maturity is here reviewed, based on 5556 Rock-Eval analyses and total organic carbon (TOC) measurements from 78 wells and 1175 vitrinite reflectance (VR) measurement from 55 wells, which makes this study the most comprehensive to date. The thermal maturity is evaluated through 1-D basin modelling of 46 wells. Statistical parameters describ-ing the distribution of TOC, hydrocarbon index (HI) and Tmax are presented for the Lower Jurassic marin

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Jeans, C. V. "Clay mineralogy of the Cretaceous strata of the British Isles." Clay Minerals 41, no. 1 (2006): 47–150. http://dx.doi.org/10.1180/0009855064110196.

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AbstractThe clay mineralogy of the Cretaceous strata of the British Isles is described and discussed within its lithostratigraphical and biostratigraphical framework using published and unpublished sources as well as 1400 new clay mineral analyses. The regional clay mineral variation is described systematically for the following strata:(1)Southern England — Purbeck Limestone Group (Berriasian/Ryazanian; Lulworth and Durlston formations), Wealden Group (Valanginian—Barremian/Aptian; Ashdown, Wadhurst Clay, Tunbridge Wells Sands, Grinstead Clay Member, Wealden Clay, Wessex and Vectis formations)

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Gradstein, Felix M., and Colin N. Waters. "Stratigraphic Guide to the Cromer Knoll, Shetland and Chalk Groups, North Sea and Norwegian Sea." Newsletters on Stratigraphy 49, no. 1 (2016). http://dx.doi.org/10.1127/nos/2016/0071.

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Dissertations / Theses on the topic "Cromer Knoll"

1

McCormick, Dominic. "Lithostratigraphy of the Cromer Knoll Group of the Puffin Area, UK Central North Sea." Thesis, University of Aberdeen, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.295625.

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This study is an evaluation of the lithostratigraphy of the Early Cretaceous Cromer Knoll Group in an area of the UK Central Graben, Central North Sea. These fine grained sediments were deposited in an open marine, clastic-dominated system. Background carbonate deposition became more dominant during periods of reduced clastic input. There were also periods of dysaerobic conditions with brief, but well defined, anoxic events, producing regionally correlateable markers. 13 wells and 650km of 2D and 3D seismic data have been used to construct detailed correlations and isochore maps. The factors g

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2

Ramnarine, Sarika Kala. "Late Cretaceous turbidites, Heidrun field, Norwegian Continental Shelf." Thesis, 2011. http://hdl.handle.net/2152/ETD-UT-2011-05-3262.

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The Heidrun field is located in the Halten Terrace of the Mid-Norwegian Continental Shelf and is one of the first giant oil fields found on the Norwegian Sea. Modern 3D seismic reflection data acquired over the field, as well as well data were used to define the key structural and stratigraphic elements within the study area. The basic geologic history of the Heidrun field is typical of most North Sea plays, and includes Triassic rift sequences that are masked by the reactivation of bounding faults that were active during the Jurassic rift phase. This rifting phase was followed by deposition o

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