FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2007456609> ?p ?o ?g. }

• W2007456609 endingPage "183" @default.
• W2007456609 startingPage "167" @default.
• W2007456609 abstract "Major revisions are proposed to the stratigraphy of the late Precambrian Longmyndian Supergroup of the Welsh Borderland. The stratigraphic relationship between it and the adjacent, late Precambrian Uriconian volcanic complex is reviewed and reinterpreted. Contrary to previous belief it is proposed that the Wentnor Group of the Longmyndian Supergroup does not overlie the Stretton Group unconformably. An apparent unconformity is interpreted as the result of post-Longmyndian tectonism. The Ragleth Tuff Formation, previously included with the Uriconian volcanic complex, is argued to be part of the Longmyndian Supergroup. The Helmeth Grit Member, previously thought to be the base of the Longmyndian Supergroup, is incorporated within the Ragleth Tuff Formation. These modifications necessitate a revision of the previously held belief that the Helmeth Grit Member is the base of the Longmyndian Supergroup which overlies the ‘Ragleth Tuffs’ of the Uriconian volcanic complex unconformably. The Ragleth Tuff Formation and the Stretton Shale Formation are thought to be faulted against the Eastern Uriconian, and the Wentnor Group is thought to be faulted against the Western Uriconian. Juxtaposition of the Longmyndian Supergroup with the Uriconian volcanic complex across faults is the result of strike-slip movements along the Church Stretton and Pontesford-Linley fault systems. Lithological and petrographical evidence suggests that the Longmyndian Supergroup is partly coeval with, and partly younger than, the Uriconian volcanic complex, which acted as a source. The Willstone Hill conglomerate, previously thought to be interbedded with the Eastern Uriconian, may be a representative of the Wentnor Group which overlies the Eastern Uriconian unconformably. As such, it may represent a late onlap of Longmyndian sediments onto the Eastern Uriconian at the margins of the Longmyndian basin. A new formation, the Linley Formation, is recognized. This occurs as fault-bounded slivers and lenses within the Pontesford-Linley fault system, and correlation with the rest of the Longmyndian is uncertain." @default.
• W2007456609 created "2016-06-24" @default.
• W2007456609 creator A5086102432 @default.
• W2007456609 date "1991-04-01" @default.
• W2007456609 modified "2023-09-25" @default.
• W2007456609 title "A revision of the stratigraphy of the longmyndian supergroup, welsh borderland, and of its relationship to the uriconian volcanic complex" @default.
• W2007456609 cites W1963858086 @default.
• W2007456609 cites W1969081475 @default.
• W2007456609 cites W1979472430 @default.
• W2007456609 cites W1987590114 @default.
• W2007456609 cites W1990831954 @default.
• W2007456609 cites W2003445906 @default.
• W2007456609 cites W2016579541 @default.
• W2007456609 cites W2024475272 @default.
• W2007456609 cites W2029922206 @default.
• W2007456609 cites W2051664514 @default.
• W2007456609 cites W2061523829 @default.
• W2007456609 cites W2063749650 @default.
• W2007456609 cites W2065463997 @default.
• W2007456609 cites W2065587463 @default.
• W2007456609 cites W2090950637 @default.
• W2007456609 cites W2102277876 @default.
• W2007456609 cites W2108625436 @default.
• W2007456609 cites W2109708218 @default.
• W2007456609 cites W2112760345 @default.
• W2007456609 cites W2113010527 @default.
• W2007456609 cites W2120509345 @default.
• W2007456609 cites W2133522038 @default.
• W2007456609 cites W2138776159 @default.
• W2007456609 cites W2499971012 @default.
• W2007456609 cites W4229895937 @default.
• W2007456609 cites W4246565617 @default.
• W2007456609 doi "https://doi.org/10.1002/gj.3350260209" @default.
• W2007456609 hasPublicationYear "1991" @default.
• W2007456609 type Work @default.
• W2007456609 sameAs 2007456609 @default.
• W2007456609 citedByCount "8" @default.
• W2007456609 countsByYear W20074566092015 @default.
• W2007456609 countsByYear W20074566092016 @default.
• W2007456609 crossrefType "journal-article" @default.
• W2007456609 hasAuthorship W2007456609A5086102432 @default.
• W2007456609 hasConcept C106804226 @default.
• W2007456609 hasConcept C109281948 @default.
• W2007456609 hasConcept C120806208 @default.
• W2007456609 hasConcept C127313418 @default.
• W2007456609 hasConcept C151730666 @default.
• W2007456609 hasConcept C173776410 @default.
• W2007456609 hasConcept C178790620 @default.
• W2007456609 hasConcept C185592680 @default.
• W2007456609 hasConcept C191735495 @default.
• W2007456609 hasConcept C192241223 @default.
• W2007456609 hasConcept C2781311116 @default.
• W2007456609 hasConcept C6494504 @default.
• W2007456609 hasConcept C64957494 @default.
• W2007456609 hasConcept C77928131 @default.
• W2007456609 hasConceptScore W2007456609C106804226 @default.
• W2007456609 hasConceptScore W2007456609C109281948 @default.
• W2007456609 hasConceptScore W2007456609C120806208 @default.
• W2007456609 hasConceptScore W2007456609C127313418 @default.
• W2007456609 hasConceptScore W2007456609C151730666 @default.
• W2007456609 hasConceptScore W2007456609C173776410 @default.
• W2007456609 hasConceptScore W2007456609C178790620 @default.
• W2007456609 hasConceptScore W2007456609C185592680 @default.
• W2007456609 hasConceptScore W2007456609C191735495 @default.
• W2007456609 hasConceptScore W2007456609C192241223 @default.
• W2007456609 hasConceptScore W2007456609C2781311116 @default.
• W2007456609 hasConceptScore W2007456609C6494504 @default.
• W2007456609 hasConceptScore W2007456609C64957494 @default.
• W2007456609 hasConceptScore W2007456609C77928131 @default.
• W2007456609 hasIssue "2" @default.
• W2007456609 hasLocation W20074566091 @default.
• W2007456609 hasOpenAccess W2007456609 @default.
• W2007456609 hasPrimaryLocation W20074566091 @default.
• W2007456609 hasRelatedWork W1893409500 @default.
• W2007456609 hasRelatedWork W1927051564 @default.
• W2007456609 hasRelatedWork W2007456609 @default.
• W2007456609 hasRelatedWork W2012022417 @default.
• W2007456609 hasRelatedWork W2062893228 @default.
• W2007456609 hasRelatedWork W2063536033 @default.
• W2007456609 hasRelatedWork W2080371369 @default.
• W2007456609 hasRelatedWork W2243694597 @default.
• W2007456609 hasRelatedWork W2410974019 @default.
• W2007456609 hasRelatedWork W2467057125 @default.
• W2007456609 hasVolume "26" @default.
• W2007456609 isParatext "false" @default.
• W2007456609 isRetracted "false" @default.
• W2007456609 magId "2007456609" @default.
• W2007456609 workType "article" @default.