FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2069403670> ?p ?o ?g. }

• W2069403670 endingPage "275" @default.
• W2069403670 startingPage "257" @default.
• W2069403670 abstract "Abstract Sandstone bodies within the Lower Old Red Sandstone (ORS) in southern Pembrokeshire exhibit variability in architecture, sediment grade and composition both spatially and temporally. Four architectural styles are observed, namely decimetre‐ to metre‐thick sheets, metre‐thick multi‐storey amalgamations, inclined‐heterolithic units and ribbon geometries. Sandstone bodies in the Freshwater East Formation are sheet‐like, heterolithic units several metres thick. An association with lingulids and wave ripples alludes to a marine influence, possibly estuarine tidal flats or storm washovers. Within the Moor Cliffs Formation, the most common sandstone bodies are centimetre‐ to metre‐thick sheets with high width‐to‐depth ratios. Fine‐grained sandstones represent sheet‐flood deposition on unconfined, planar surfaces, whereas coarser‐grained sandstones constitute distinctive amalgamations of discrete flood events, reflecting either a change in provenance or tectonic influence. Clear incision of coarse‐grained, multi‐storey units within the Inter‐Tuff Moor Cliffs Formation reflects a change in relative sea‐level, possibly tectonically induced. The base of the Conigar Pit Sandstone Member (CPSM) is marked by a distinctive, exotic‐clast conglomerate defining the base to heterolithic, lateral‐accretion bedsets and sandstone sheets. This association defines a significant influx of coarse‐grained sediment post‐Chapel Point Calcrete formation, an interval of presumed topographic stability across the Anglo‐Welsh Basin. This influx must reflect rejuvenation of source regions, with changes in base‐level reflecting either eustatic or tectonic influences. Commonly observed in the CPSM are fine‐grained, inclined‐heterolithic bedsets recording deposition by highly sinuous rivers with flashy discharge. Up‐sequence within the CPSM are metre‐thick, multi‐storey amalgamations of predominatly trough cross‐stratified medium‐ to coarse‐grained sandstone. It is likely that these units are genetically related to contemporaneous decimetre‐thick sandstone sheets, the latter being ‘splay’ events marginal to the main channel axis. The interbedding of multi‐storey sandstones and fine‐grained laterally accreted units reflects changes in provenance, slope and/or climate. Thickness variations within the Lower ORS detail significant thickening of all units northward into the Benton Fault. It seems likely that this thickening reflects variable accommodation space development associated with active growth along this and other WNW–ESE‐trending faults, and migration of channel belts toward the footwall. Copyright © 2004 John Wiley & Sons, Ltd." @default.
• W2069403670 created "2016-06-24" @default.
• W2069403670 creator A5027314156 @default.
• W2069403670 creator A5091070402 @default.
• W2069403670 date "2004-07-01" @default.
• W2069403670 modified "2023-10-13" @default.
• W2069403670 title "Variable alluvial sandstone architecture within the Lower Old Red Sandstone, southwest Wales" @default.
• W2069403670 cites W1568768969 @default.
• W2069403670 cites W1590196129 @default.
• W2069403670 cites W1608274608 @default.
• W2069403670 cites W1853841102 @default.
• W2069403670 cites W1973426546 @default.
• W2069403670 cites W1991764655 @default.
• W2069403670 cites W1994958984 @default.
• W2069403670 cites W1996585223 @default.
• W2069403670 cites W2010797300 @default.
• W2069403670 cites W2016533866 @default.
• W2069403670 cites W2024987335 @default.
• W2069403670 cites W2031197673 @default.
• W2069403670 cites W2037409271 @default.
• W2069403670 cites W2037788431 @default.
• W2069403670 cites W2064536983 @default.
• W2069403670 cites W2074438535 @default.
• W2069403670 cites W2078690541 @default.
• W2069403670 cites W2079049513 @default.
• W2069403670 cites W2099615076 @default.
• W2069403670 cites W2119131467 @default.
• W2069403670 cites W2128600920 @default.
• W2069403670 cites W2137313425 @default.
• W2069403670 cites W2140597351 @default.
• W2069403670 cites W2149760466 @default.
• W2069403670 cites W2152694150 @default.
• W2069403670 cites W2163466829 @default.
• W2069403670 cites W2169222276 @default.
• W2069403670 cites W2171243662 @default.
• W2069403670 cites W2313464505 @default.
• W2069403670 cites W2333799139 @default.
• W2069403670 doi "https://doi.org/10.1002/gj.993" @default.
• W2069403670 hasPublicationYear "2004" @default.
• W2069403670 type Work @default.
• W2069403670 sameAs 2069403670 @default.
• W2069403670 citedByCount "24" @default.
• W2069403670 countsByYear W20694036702012 @default.
• W2069403670 countsByYear W20694036702014 @default.
• W2069403670 countsByYear W20694036702017 @default.
• W2069403670 countsByYear W20694036702018 @default.
• W2069403670 countsByYear W20694036702019 @default.
• W2069403670 countsByYear W20694036702020 @default.
• W2069403670 countsByYear W20694036702021 @default.
• W2069403670 countsByYear W20694036702022 @default.
• W2069403670 crossrefType "journal-article" @default.
• W2069403670 hasAuthorship W2069403670A5027314156 @default.
• W2069403670 hasAuthorship W2069403670A5091070402 @default.
• W2069403670 hasConcept C106804226 @default.
• W2069403670 hasConcept C109007969 @default.
• W2069403670 hasConcept C114793014 @default.
• W2069403670 hasConcept C127313418 @default.
• W2069403670 hasConcept C138170599 @default.
• W2069403670 hasConcept C151730666 @default.
• W2069403670 hasConcept C2780049196 @default.
• W2069403670 hasConcept C2816523 @default.
• W2069403670 hasConcept C64297162 @default.
• W2069403670 hasConceptScore W2069403670C106804226 @default.
• W2069403670 hasConceptScore W2069403670C109007969 @default.
• W2069403670 hasConceptScore W2069403670C114793014 @default.
• W2069403670 hasConceptScore W2069403670C127313418 @default.
• W2069403670 hasConceptScore W2069403670C138170599 @default.
• W2069403670 hasConceptScore W2069403670C151730666 @default.
• W2069403670 hasConceptScore W2069403670C2780049196 @default.
• W2069403670 hasConceptScore W2069403670C2816523 @default.
• W2069403670 hasConceptScore W2069403670C64297162 @default.
• W2069403670 hasIssue "3-4" @default.
• W2069403670 hasLocation W20694036701 @default.
• W2069403670 hasOpenAccess W2069403670 @default.
• W2069403670 hasPrimaryLocation W20694036701 @default.
• W2069403670 hasRelatedWork W1577212064 @default.
• W2069403670 hasRelatedWork W2102065875 @default.
• W2069403670 hasRelatedWork W2110396674 @default.
• W2069403670 hasRelatedWork W2120030462 @default.
• W2069403670 hasRelatedWork W2120244432 @default.
• W2069403670 hasRelatedWork W2125869210 @default.
• W2069403670 hasRelatedWork W2342908875 @default.
• W2069403670 hasRelatedWork W2349796316 @default.
• W2069403670 hasRelatedWork W2391449514 @default.
• W2069403670 hasRelatedWork W3012092027 @default.
• W2069403670 hasVolume "39" @default.
• W2069403670 isParatext "false" @default.
• W2069403670 isRetracted "false" @default.
• W2069403670 magId "2069403670" @default.
• W2069403670 workType "article" @default.