Matches in SemOpenAlex for { <https://semopenalex.org/work/W2014122600> ?p ?o ?g. }
Showing items 1 to 78 of
78
with 100 items per page.
- W2014122600 endingPage "82" @default.
- W2014122600 startingPage "74" @default.
- W2014122600 abstract "Bathonian to Oxfordian strata occur onshore in two principal locations over 30 km apart on the coast of the Moray Firth, at Brora and Balintore. The existing lithostratigraphy has the same formation names applied to both successions despite profound differences, exemplified in their schemes of local members. Furthermore, three of the formation names include the same place name, and use obsolete lithological terms. We consider that all the Bathonian to Oxfordian members are satisfactory, and propose their retention with original names, with one exception, to provide continuity with the superseded formational scheme. We propose retention of the Brora Coal Formation as currently defined. The Brora Argillaceous, Brora Arenaceous and Balintore formations at Brora are unsatisfactory in a modern context and we propose: a new Strathsteven Mudstone Formation, which is mudstone-dominated, and generally coarsens-upwards. a Clynekirkton Sandstone Formation, which is sandstone-dominated and generally coarsens upwards. This formation scheme employs unique geographical names and modern and appropriate lithological terminology. Furthermore, the boundary between the Strathsteven and Clynekirkton formations is placed at a junction that is a change from mud- and silt-dominated lithologies to silt- and fine- and medium-grained sand and is mappable. We consider that the Callovian–Oxfordian succession at Balintore should be assigned to a single formation, viz. the revised Balintore Formation. Apart from the basal Brora Roof Bed, the succession at Balintore does not lithologically resemble that at Brora, and the scheme of the Brora Argillaceous Formation, Brora Arenaceous Formation, and the Balintore Formation as previously defined is unworkable here." @default.
- W2014122600 created "2016-06-24" @default.
- W2014122600 creator A5011190539 @default.
- W2014122600 creator A5058137435 @default.
- W2014122600 date "2014-01-01" @default.
- W2014122600 modified "2023-09-23" @default.
- W2014122600 title "A revision of the Jurassic (Bathonian to Oxfordian) lithostratigraphy of the onshore Moray Firth Basin, north-east Scotland" @default.
- W2014122600 cites W1964714812 @default.
- W2014122600 cites W1985046302 @default.
- W2014122600 cites W1987566618 @default.
- W2014122600 cites W2001899608 @default.
- W2014122600 cites W2018063177 @default.
- W2014122600 cites W2054847857 @default.
- W2014122600 cites W2093868116 @default.
- W2014122600 cites W2100045670 @default.
- W2014122600 cites W2107492372 @default.
- W2014122600 cites W2112377341 @default.
- W2014122600 cites W2116931971 @default.
- W2014122600 cites W2123549864 @default.
- W2014122600 cites W2164419187 @default.
- W2014122600 cites W2326320827 @default.
- W2014122600 doi "https://doi.org/10.1016/j.pgeola.2013.08.004" @default.
- W2014122600 hasPublicationYear "2014" @default.
- W2014122600 type Work @default.
- W2014122600 sameAs 2014122600 @default.
- W2014122600 citedByCount "4" @default.
- W2014122600 countsByYear W20141226002017 @default.
- W2014122600 countsByYear W20141226002023 @default.
- W2014122600 crossrefType "journal-article" @default.
- W2014122600 hasAuthorship W2014122600A5011190539 @default.
- W2014122600 hasAuthorship W2014122600A5058137435 @default.
- W2014122600 hasBestOaLocation W20141226002 @default.
- W2014122600 hasConcept C109007969 @default.
- W2014122600 hasConcept C114793014 @default.
- W2014122600 hasConcept C122792734 @default.
- W2014122600 hasConcept C127313418 @default.
- W2014122600 hasConcept C150117547 @default.
- W2014122600 hasConcept C151730666 @default.
- W2014122600 hasConcept C161222754 @default.
- W2014122600 hasConcept C18903297 @default.
- W2014122600 hasConcept C2778371416 @default.
- W2014122600 hasConcept C2779343474 @default.
- W2014122600 hasConcept C40616122 @default.
- W2014122600 hasConcept C86803240 @default.
- W2014122600 hasConceptScore W2014122600C109007969 @default.
- W2014122600 hasConceptScore W2014122600C114793014 @default.
- W2014122600 hasConceptScore W2014122600C122792734 @default.
- W2014122600 hasConceptScore W2014122600C127313418 @default.
- W2014122600 hasConceptScore W2014122600C150117547 @default.
- W2014122600 hasConceptScore W2014122600C151730666 @default.
- W2014122600 hasConceptScore W2014122600C161222754 @default.
- W2014122600 hasConceptScore W2014122600C18903297 @default.
- W2014122600 hasConceptScore W2014122600C2778371416 @default.
- W2014122600 hasConceptScore W2014122600C2779343474 @default.
- W2014122600 hasConceptScore W2014122600C40616122 @default.
- W2014122600 hasConceptScore W2014122600C86803240 @default.
- W2014122600 hasIssue "1" @default.
- W2014122600 hasLocation W20141226001 @default.
- W2014122600 hasLocation W20141226002 @default.
- W2014122600 hasOpenAccess W2014122600 @default.
- W2014122600 hasPrimaryLocation W20141226001 @default.
- W2014122600 hasRelatedWork W1547281 @default.
- W2014122600 hasRelatedWork W1758396658 @default.
- W2014122600 hasRelatedWork W1978330345 @default.
- W2014122600 hasRelatedWork W1978501348 @default.
- W2014122600 hasRelatedWork W2104696163 @default.
- W2014122600 hasRelatedWork W2136182680 @default.
- W2014122600 hasRelatedWork W2325222095 @default.
- W2014122600 hasRelatedWork W2726974038 @default.
- W2014122600 hasRelatedWork W3094795434 @default.
- W2014122600 hasRelatedWork W4282582161 @default.
- W2014122600 hasVolume "125" @default.
- W2014122600 isParatext "false" @default.
- W2014122600 isRetracted "false" @default.
- W2014122600 magId "2014122600" @default.
- W2014122600 workType "article" @default.