FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W148103666> ?p ?o ?g. }

• W148103666 endingPage "238" @default.
• W148103666 startingPage "221" @default.
• W148103666 abstract "Abstract Middle Jurassic - Early Cretaceous strata are a target for oil and gas exploration in the Dutch offshore. During the initial stages of the ‘Late Jurassic’ offshore exploration, various oil fields and a few gas fields were discovered of which only one, the F3-FB field, proved to be economically viable. In the Northern Offshore of the Netherlands, latest Middle Jurassic (Callovian) - earliest Cretaceous (Ryazanian) strata are mostly limited to the Dutch Central Graben and Terschelling basins. Outside the Dutch Central Graben and the Terschelling Basin only thin veneers of these strata occur on the fringing highs such as the Schill Grund High and the Step Graben. The geology of this non-marine to shallow marine succession is complex. The combination of lateral facies changes, repetitive log and facies characteristics in time, sea-level and climate changes, salt tectonics and structural compartmentalisation hamper straightforward seismic interpretation and log correlation. The large number of lithostratigraphic units defined in the Stratigraphic Nomenclature of the Netherlands illustrates the complexity of this time-interval. In recent years, new biostratigraphic techniques and newly acquired stratigraphic data led to the identification of a series of events which can be related to the tectonic, climatic, environmental and stratigraphic development of the ‘Late Jurassic’ in the Dutch Central Graben and Terschelling basins. Based on these data, three stratigraphic sequences can be recognized. Sequence 1 (Callovian - earliest Kimmeridgian) records the initiation of the Dutch Central Graben, Sequence 2 (early Kimmeridgian - early Portlandian) that of the initiation of the Terschelling Basin. During sequence 3 (late Portlandian - Ryazanian) the Dutch offshore was draped by a regional transgression. These insights have directly impact on the exploration potential, which is discussed in two play concepts. The first is a strat-trap play in the fluvial/paralic sediments of Sequence 1 in the lows between the graben boundary and salt domes. The second example is the Spiculite play, which comprises a bioclastic sandstone reservoir at the top of a dome with a 4-way dip closure. These two examples highlight the necessity of understanding the paleoenvironment and geography for assessing the future exploration potential." @default.
• W148103666 created "2016-06-24" @default.
• W148103666 creator A5000405726 @default.
• W148103666 creator A5021045397 @default.
• W148103666 creator A5037213164 @default.
• W148103666 creator A5083928626 @default.
• W148103666 date "2006-09-01" @default.
• W148103666 modified "2023-09-30" @default.
• W148103666 title "New stratigraphic insights in the ’Late Jurassic’ of the Southern Central North Sea Graben and Terschelling Basin (Dutch Offshore) and related exploration potential" @default.
• W148103666 cites W2008900622 @default.
• W148103666 cites W2024176565 @default.
• W148103666 cites W2063800269 @default.
• W148103666 cites W2092588143 @default.
• W148103666 cites W2141839758 @default.
• W148103666 cites W4232328127 @default.
• W148103666 doi "https://doi.org/10.1017/s001677460002148x" @default.
• W148103666 hasPublicationYear "2006" @default.
• W148103666 type Work @default.
• W148103666 sameAs 148103666 @default.
• W148103666 citedByCount "21" @default.
• W148103666 countsByYear W1481036662012 @default.
• W148103666 countsByYear W1481036662013 @default.
• W148103666 countsByYear W1481036662014 @default.
• W148103666 countsByYear W1481036662016 @default.
• W148103666 countsByYear W1481036662017 @default.
• W148103666 countsByYear W1481036662018 @default.
• W148103666 countsByYear W1481036662019 @default.
• W148103666 countsByYear W1481036662020 @default.
• W148103666 countsByYear W1481036662021 @default.
• W148103666 countsByYear W1481036662022 @default.
• W148103666 countsByYear W1481036662023 @default.
• W148103666 crossrefType "journal-article" @default.
• W148103666 hasAuthorship W148103666A5000405726 @default.
• W148103666 hasAuthorship W148103666A5021045397 @default.
• W148103666 hasAuthorship W148103666A5037213164 @default.
• W148103666 hasAuthorship W148103666A5083928626 @default.
• W148103666 hasBestOaLocation W1481036661 @default.
• W148103666 hasConcept C109007969 @default.
• W148103666 hasConcept C12294951 @default.
• W148103666 hasConcept C127313418 @default.
• W148103666 hasConcept C146588470 @default.
• W148103666 hasConcept C151730666 @default.
• W148103666 hasConcept C166839181 @default.
• W148103666 hasConcept C179158327 @default.
• W148103666 hasConcept C2778112365 @default.
• W148103666 hasConcept C54355233 @default.
• W148103666 hasConcept C6363049 @default.
• W148103666 hasConcept C77928131 @default.
• W148103666 hasConcept C86803240 @default.
• W148103666 hasConceptScore W148103666C109007969 @default.
• W148103666 hasConceptScore W148103666C12294951 @default.
• W148103666 hasConceptScore W148103666C127313418 @default.
• W148103666 hasConceptScore W148103666C146588470 @default.
• W148103666 hasConceptScore W148103666C151730666 @default.
• W148103666 hasConceptScore W148103666C166839181 @default.
• W148103666 hasConceptScore W148103666C179158327 @default.
• W148103666 hasConceptScore W148103666C2778112365 @default.
• W148103666 hasConceptScore W148103666C54355233 @default.
• W148103666 hasConceptScore W148103666C6363049 @default.
• W148103666 hasConceptScore W148103666C77928131 @default.
• W148103666 hasConceptScore W148103666C86803240 @default.
• W148103666 hasIssue "3" @default.
• W148103666 hasLocation W1481036661 @default.
• W148103666 hasOpenAccess W148103666 @default.
• W148103666 hasPrimaryLocation W1481036661 @default.
• W148103666 hasRelatedWork W1983158600 @default.
• W148103666 hasRelatedWork W1994488541 @default.
• W148103666 hasRelatedWork W2049866890 @default.
• W148103666 hasRelatedWork W2081758660 @default.
• W148103666 hasRelatedWork W2325222095 @default.
• W148103666 hasRelatedWork W2349785325 @default.
• W148103666 hasRelatedWork W2351005350 @default.
• W148103666 hasRelatedWork W2361783714 @default.
• W148103666 hasRelatedWork W2916446095 @default.
• W148103666 hasRelatedWork W4237302839 @default.
• W148103666 hasVolume "85" @default.
• W148103666 isParatext "false" @default.
• W148103666 isRetracted "false" @default.
• W148103666 magId "148103666" @default.
• W148103666 workType "article" @default.