Matches in SemOpenAlex for { <https://semopenalex.org/work/W4256297312> ?p ?o ?g. }
Showing items 1 to 74 of
74
with 100 items per page.
- W4256297312 endingPage "140" @default.
- W4256297312 startingPage "121" @default.
- W4256297312 abstract "Mud-mound complexes identified within the early to middle Ashgill Cystoid Limestone Formation of northeastern Spain are the first fossil build-ups to be described in the high latitude north-facing margin of Gondwana. Mud-mound complexes comprise individual lenticular mounds (composed of floatstones, cephalopod-rich mudstones and cementstones), flanks and intermound deposits (including pelmatozoan packstones and floatstones). The small mounds are mainly composed of bryozoans, cystoids and crinoids, and were developed on outer ramp environments. Mound initiation depended upon the stabilization and colonization of densely packed lenses of pelmatozoan-rich sediments. In a mid-ramp setting, pelmatozoan–bryozoan meadows were episodically degraded by common wave- and storm-induced processes, the development of semi-consolidated substrates, and the periodic influx of terrigenous material. Finally, during the Hirnantian regression, the Iberian mixed (carbonate–siliciclastic) platform was exposed to subaerial conditions sufficiently for erosion and karstification to occur. From a palaeogeographical point of view, the pattern of the Ashgill Iberian platform deposition is characterized by episodic exclusion of carbonates from most nearshore environments by a shoreline source of siliciclastic sediments. A similar interpretation to that made on the Iberian Cystoid Limestone Formation, in terms of gradual proximality–distality changes, is proposed for comparable facies types in Ashgill limestones described in southwestern Europe. © 1998 John Wiley & Sons, Ltd." @default.
- W4256297312 created "2022-05-12" @default.
- W4256297312 creator A5012900986 @default.
- W4256297312 creator A5050478380 @default.
- W4256297312 creator A5090888488 @default.
- W4256297312 date "1998-04-01" @default.
- W4256297312 modified "2023-10-01" @default.
- W4256297312 title "High‐latitude pelmatozoan–bryozoan mud‐mounds from the late Ordovician northern Gondwana platform" @default.
- W4256297312 doi "https://doi.org/10.1002/(sici)1099-1034(1998040)33:2<121::aid-gj780>3.3.co;2-4" @default.
- W4256297312 hasPublicationYear "1998" @default.
- W4256297312 type Work @default.
- W4256297312 citedByCount "0" @default.
- W4256297312 crossrefType "journal-article" @default.
- W4256297312 hasAuthorship W4256297312A5012900986 @default.
- W4256297312 hasAuthorship W4256297312A5050478380 @default.
- W4256297312 hasAuthorship W4256297312A5090888488 @default.
- W4256297312 hasConcept C104873425 @default.
- W4256297312 hasConcept C109007969 @default.
- W4256297312 hasConcept C127313418 @default.
- W4256297312 hasConcept C146588470 @default.
- W4256297312 hasConcept C151730666 @default.
- W4256297312 hasConcept C18903297 @default.
- W4256297312 hasConcept C191897082 @default.
- W4256297312 hasConcept C192562407 @default.
- W4256297312 hasConcept C199285206 @default.
- W4256297312 hasConcept C2776386860 @default.
- W4256297312 hasConcept C2780659211 @default.
- W4256297312 hasConcept C2781148125 @default.
- W4256297312 hasConcept C6494504 @default.
- W4256297312 hasConcept C76947770 @default.
- W4256297312 hasConcept C77271252 @default.
- W4256297312 hasConcept C84983702 @default.
- W4256297312 hasConcept C86803240 @default.
- W4256297312 hasConcept C91442348 @default.
- W4256297312 hasConcept C93257316 @default.
- W4256297312 hasConceptScore W4256297312C104873425 @default.
- W4256297312 hasConceptScore W4256297312C109007969 @default.
- W4256297312 hasConceptScore W4256297312C127313418 @default.
- W4256297312 hasConceptScore W4256297312C146588470 @default.
- W4256297312 hasConceptScore W4256297312C151730666 @default.
- W4256297312 hasConceptScore W4256297312C18903297 @default.
- W4256297312 hasConceptScore W4256297312C191897082 @default.
- W4256297312 hasConceptScore W4256297312C192562407 @default.
- W4256297312 hasConceptScore W4256297312C199285206 @default.
- W4256297312 hasConceptScore W4256297312C2776386860 @default.
- W4256297312 hasConceptScore W4256297312C2780659211 @default.
- W4256297312 hasConceptScore W4256297312C2781148125 @default.
- W4256297312 hasConceptScore W4256297312C6494504 @default.
- W4256297312 hasConceptScore W4256297312C76947770 @default.
- W4256297312 hasConceptScore W4256297312C77271252 @default.
- W4256297312 hasConceptScore W4256297312C84983702 @default.
- W4256297312 hasConceptScore W4256297312C86803240 @default.
- W4256297312 hasConceptScore W4256297312C91442348 @default.
- W4256297312 hasConceptScore W4256297312C93257316 @default.
- W4256297312 hasIssue "2" @default.
- W4256297312 hasLocation W42562973121 @default.
- W4256297312 hasOpenAccess W4256297312 @default.
- W4256297312 hasPrimaryLocation W42562973121 @default.
- W4256297312 hasRelatedWork W1964406565 @default.
- W4256297312 hasRelatedWork W1994180156 @default.
- W4256297312 hasRelatedWork W2023032996 @default.
- W4256297312 hasRelatedWork W2030407912 @default.
- W4256297312 hasRelatedWork W2031964123 @default.
- W4256297312 hasRelatedWork W2091960207 @default.
- W4256297312 hasRelatedWork W2119866941 @default.
- W4256297312 hasRelatedWork W3134169058 @default.
- W4256297312 hasRelatedWork W3134462804 @default.
- W4256297312 hasRelatedWork W3172985626 @default.
- W4256297312 hasVolume "33" @default.
- W4256297312 isParatext "false" @default.
- W4256297312 isRetracted "false" @default.
- W4256297312 workType "article" @default.