Matches in SemOpenAlex for { <https://semopenalex.org/work/W3173861486> ?p ?o ?g. }
Showing items 1 to 78 of
78
with 100 items per page.
- W3173861486 abstract "The Latium-Abruzzi platform is a well-known large shallow water domain of Central Apennines, however the reconstruction of geometry and evolution of its western margin remains poorly known because it was involved into the out-of sequence Olevano-Antrodoco thrust system. The investigated area is located in the Prenestini Mountains, at the southernmost portion of the Sabina Domain, westward of the large Latium-Abruzzi Platform domain. Here isolated outcrops of Cretaceous to Neogene carbonate successions exhibit a complex history of shallow water carbonate production, drowning, erosive phases and condensed sedimentation within a tectonic-eustatic-controlled carbonate platform marginal domain. Stratigraphic and facies analyses allowed to recognize two main fault block platforms, respectively South-Eastern Prenestini (SEP) and South Western Prenestini (SWP) platforms which in turn have been disjointed into smaller blocks. The displacement of all these blocks can be referred to the widely recognized upper Cretaceous extensional tectonic phase.In these Platforms, during the Paleocene-Eocene interval, the onset of pelagic environment, and the related condensed pelagites, coincides with main relative sea-level rise, whereas during the following falling stage the depositional surface, coming into the wave abrasion zone, was affected by high hydrodynamic energy and the produced pelagic carbonate was swept away or trapped in local depressions and/or within the fractures forming the neptunian dykes. The coarse-grained material, produced by the erosion of the fractured and articulated Cretaceous substrate, was reworked together with fragments of pelagites to form lenses of polygenic conglomerates resting on top of the Cretaceuos platform carbonates. In the Chattian to Aquitanian time interval, short phases of shallow water carbonate production were established during the sea-level fall, as testified by the larger benthic foraminiferal-rich carbonates, followed by erosion and reworking of the already produced sediments into the northern and more deep platform-to-basin zones.Successively, during the Aquitanian to Serravallian time interval, an homoclinal ramp hosting the Guadagnolo Fm, developed on the drowned fault block platforms, suggesting that during the Neogene the articulated substrate was roughly smoothed by the onlapping marly deposits of the basal Guadagnolo Fm and could accommodate the subsequent bioclastic sedimentation allowing the development of a carbonate ramp depositional profile." @default.
- W3173861486 created "2021-07-05" @default.
- W3173861486 creator A5039858222 @default.
- W3173861486 creator A5055218291 @default.
- W3173861486 creator A5064410252 @default.
- W3173861486 date "2020-06-30" @default.
- W3173861486 modified "2023-09-23" @default.
- W3173861486 title "Late Cretaceous to early Miocene evolution of the Southern Prenestini Mountains (Central Apennines): from fault-block platforms to carbonate ramp" @default.
- W3173861486 doi "https://doi.org/10.3304/jmes.2020.16860" @default.
- W3173861486 hasPublicationYear "2020" @default.
- W3173861486 type Work @default.
- W3173861486 sameAs 3173861486 @default.
- W3173861486 citedByCount "2" @default.
- W3173861486 countsByYear W31738614862021 @default.
- W3173861486 crossrefType "journal-article" @default.
- W3173861486 hasAuthorship W3173861486A5039858222 @default.
- W3173861486 hasAuthorship W3173861486A5055218291 @default.
- W3173861486 hasAuthorship W3173861486A5064410252 @default.
- W3173861486 hasConcept C109007969 @default.
- W3173861486 hasConcept C12294951 @default.
- W3173861486 hasConcept C126753816 @default.
- W3173861486 hasConcept C127313418 @default.
- W3173861486 hasConcept C146588470 @default.
- W3173861486 hasConcept C151730666 @default.
- W3173861486 hasConcept C169212394 @default.
- W3173861486 hasConcept C175551986 @default.
- W3173861486 hasConcept C191897082 @default.
- W3173861486 hasConcept C192562407 @default.
- W3173861486 hasConcept C203457885 @default.
- W3173861486 hasConcept C27492601 @default.
- W3173861486 hasConcept C2778609275 @default.
- W3173861486 hasConcept C2780659211 @default.
- W3173861486 hasConcept C50682988 @default.
- W3173861486 hasConcept C77928131 @default.
- W3173861486 hasConceptScore W3173861486C109007969 @default.
- W3173861486 hasConceptScore W3173861486C12294951 @default.
- W3173861486 hasConceptScore W3173861486C126753816 @default.
- W3173861486 hasConceptScore W3173861486C127313418 @default.
- W3173861486 hasConceptScore W3173861486C146588470 @default.
- W3173861486 hasConceptScore W3173861486C151730666 @default.
- W3173861486 hasConceptScore W3173861486C169212394 @default.
- W3173861486 hasConceptScore W3173861486C175551986 @default.
- W3173861486 hasConceptScore W3173861486C191897082 @default.
- W3173861486 hasConceptScore W3173861486C192562407 @default.
- W3173861486 hasConceptScore W3173861486C203457885 @default.
- W3173861486 hasConceptScore W3173861486C27492601 @default.
- W3173861486 hasConceptScore W3173861486C2778609275 @default.
- W3173861486 hasConceptScore W3173861486C2780659211 @default.
- W3173861486 hasConceptScore W3173861486C50682988 @default.
- W3173861486 hasConceptScore W3173861486C77928131 @default.
- W3173861486 hasLocation W31738614861 @default.
- W3173861486 hasOpenAccess W3173861486 @default.
- W3173861486 hasPrimaryLocation W31738614861 @default.
- W3173861486 hasRelatedWork W141697046 @default.
- W3173861486 hasRelatedWork W1497967409 @default.
- W3173861486 hasRelatedWork W1885514292 @default.
- W3173861486 hasRelatedWork W2000100117 @default.
- W3173861486 hasRelatedWork W2024259086 @default.
- W3173861486 hasRelatedWork W2055826656 @default.
- W3173861486 hasRelatedWork W2085327040 @default.
- W3173861486 hasRelatedWork W2123988488 @default.
- W3173861486 hasRelatedWork W2153098560 @default.
- W3173861486 hasRelatedWork W252250607 @default.
- W3173861486 hasRelatedWork W2739450040 @default.
- W3173861486 hasRelatedWork W2743267013 @default.
- W3173861486 hasRelatedWork W2756635838 @default.
- W3173861486 hasRelatedWork W2810069022 @default.
- W3173861486 hasRelatedWork W2965829192 @default.
- W3173861486 hasRelatedWork W2977507646 @default.
- W3173861486 hasRelatedWork W2981980747 @default.
- W3173861486 hasRelatedWork W3097065451 @default.
- W3173861486 hasRelatedWork W81898466 @default.
- W3173861486 hasRelatedWork W2510403839 @default.
- W3173861486 hasVolume "12" @default.
- W3173861486 isParatext "false" @default.
- W3173861486 isRetracted "false" @default.
- W3173861486 magId "3173861486" @default.
- W3173861486 workType "article" @default.