Matches in SemOpenAlex for { <https://semopenalex.org/work/W2094405087> ?p ?o ?g. }
Showing items 1 to 75 of
75
with 100 items per page.
- W2094405087 endingPage "10" @default.
- W2094405087 startingPage "1" @default.
- W2094405087 abstract "New seismic mapping of Skagerrak reveals eight structural provinces. In particular, the Skagerrak Graben appears to be the continuation of the Oslo Graben. The Skagerrak Graben is defined by two major Late Paleozoic faults trending northeast-southwest connecting with the faults bounding the Oslo Graben. Extensive rotated block faulting is observed within the graben and a thickness of more than 2 s TWT of Lower Paleozoic sediments has been preserved. Along the boundary faults sediments of probable Late Paleozoic age have been deposited as erosional products from the fault scarps and a central uplifted area. A substantial part of these sediments may have a volcaniclastic origin. The Skagerrak Graben continues to the north as a province of igneous rocks exposed at the sea floor with Precambrian basement on either side. The Skagerrak Graben is flanked by small half grabens containing probable Early Paleozoic sediments indicating that a wider area was involved in the rift process. The formation of the Skagerrak Graben is related to the dextral strike-slip movements along the Sorgenfrei-Tornquist Zone in Late Paleozoic time. The Kimmerian extensional movements along this zone indicate, however, a decoupling of the Skagerrak Graben at this time. Only minor inversion in the southwestern part of the Skagerrak Graben reflects the major inversion tectonism along the Sorgenfrei-Tornquist Zone in Late Cretaceous-Early Tertiary times." @default.
- W2094405087 created "2016-06-24" @default.
- W2094405087 creator A5004095776 @default.
- W2094405087 creator A5038600295 @default.
- W2094405087 creator A5058309973 @default.
- W2094405087 creator A5088165332 @default.
- W2094405087 date "1990-06-01" @default.
- W2094405087 modified "2023-10-18" @default.
- W2094405087 title "Skagerrak Graben—the offshore continuation of the Oslo Graben" @default.
- W2094405087 cites W2082773656 @default.
- W2094405087 cites W2125741113 @default.
- W2094405087 cites W2146466173 @default.
- W2094405087 cites W2178484906 @default.
- W2094405087 cites W4211228162 @default.
- W2094405087 doi "https://doi.org/10.1016/0040-1951(90)90456-i" @default.
- W2094405087 hasPublicationYear "1990" @default.
- W2094405087 type Work @default.
- W2094405087 sameAs 2094405087 @default.
- W2094405087 citedByCount "40" @default.
- W2094405087 countsByYear W20944050872012 @default.
- W2094405087 countsByYear W20944050872013 @default.
- W2094405087 countsByYear W20944050872014 @default.
- W2094405087 countsByYear W20944050872018 @default.
- W2094405087 countsByYear W20944050872020 @default.
- W2094405087 countsByYear W20944050872022 @default.
- W2094405087 crossrefType "journal-article" @default.
- W2094405087 hasAuthorship W2094405087A5004095776 @default.
- W2094405087 hasAuthorship W2094405087A5038600295 @default.
- W2094405087 hasAuthorship W2094405087A5058309973 @default.
- W2094405087 hasAuthorship W2094405087A5088165332 @default.
- W2094405087 hasConcept C127313418 @default.
- W2094405087 hasConcept C13106087 @default.
- W2094405087 hasConcept C151730666 @default.
- W2094405087 hasConcept C165205528 @default.
- W2094405087 hasConcept C166839181 @default.
- W2094405087 hasConcept C175551986 @default.
- W2094405087 hasConcept C2776074449 @default.
- W2094405087 hasConcept C4404100 @default.
- W2094405087 hasConcept C50047906 @default.
- W2094405087 hasConcept C50682988 @default.
- W2094405087 hasConcept C69168840 @default.
- W2094405087 hasConcept C77928131 @default.
- W2094405087 hasConceptScore W2094405087C127313418 @default.
- W2094405087 hasConceptScore W2094405087C13106087 @default.
- W2094405087 hasConceptScore W2094405087C151730666 @default.
- W2094405087 hasConceptScore W2094405087C165205528 @default.
- W2094405087 hasConceptScore W2094405087C166839181 @default.
- W2094405087 hasConceptScore W2094405087C175551986 @default.
- W2094405087 hasConceptScore W2094405087C2776074449 @default.
- W2094405087 hasConceptScore W2094405087C4404100 @default.
- W2094405087 hasConceptScore W2094405087C50047906 @default.
- W2094405087 hasConceptScore W2094405087C50682988 @default.
- W2094405087 hasConceptScore W2094405087C69168840 @default.
- W2094405087 hasConceptScore W2094405087C77928131 @default.
- W2094405087 hasIssue "1" @default.
- W2094405087 hasLocation W20944050871 @default.
- W2094405087 hasOpenAccess W2094405087 @default.
- W2094405087 hasPrimaryLocation W20944050871 @default.
- W2094405087 hasRelatedWork W1969919599 @default.
- W2094405087 hasRelatedWork W2047962349 @default.
- W2094405087 hasRelatedWork W2077470026 @default.
- W2094405087 hasRelatedWork W2143947177 @default.
- W2094405087 hasRelatedWork W2221269502 @default.
- W2094405087 hasRelatedWork W2302763214 @default.
- W2094405087 hasRelatedWork W2391726478 @default.
- W2094405087 hasRelatedWork W3004842966 @default.
- W2094405087 hasRelatedWork W4231242021 @default.
- W2094405087 hasRelatedWork W845394309 @default.
- W2094405087 hasVolume "178" @default.
- W2094405087 isParatext "false" @default.
- W2094405087 isRetracted "false" @default.
- W2094405087 magId "2094405087" @default.
- W2094405087 workType "article" @default.