FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4213431388> ?p ?o ?g. }

• W4213431388 endingPage "106106" @default.
• W4213431388 startingPage "106106" @default.
• W4213431388 abstract "The Norian succession of the Southern Alps of Italy stores thick successions of resedimented basinal carbonates (Zorzino Limestone) that were deposited in fault-controlled, anoxic, intraplatform basins developed within a vast inner platform domain (Dolomia Principale). To characterise the basinal facies, to define their distribution within these basins and to identify depositional processes, four stratigraphic logs covering about 2000 m of total stratigraphic thickness from proximal to distal basinal settings were described bed by bed. Eight different lithofacies organised in 11 bed types were identified according to sedimentary structures, texture, and composition: each bed (about 4500 beds in total) was measured individually at cm scale and classified in one of the 11 bed types. Distribution of bed types in terms of events (i.e. number of beds) and cumulative thickness (i.e. volume of sediments produced by the different depositional processes) in the four selected logs change from the proximal to the distal parts of the basin, reflecting the existence of diverse dominant depositional processes at different places within the intraplatform basins. Bed by bed analyses of thick stratigraphic logs provide important hints about the distribution of different types of depositional processes, from proximal to distal basin. Frequent slump folds and mass flow deposits, with clasts mostly deriving from the slope facies itself, indicate instability of the slope. Sediment composition and facies types document a major role played by the reworking of primary deposits formed along the slope: basinal facies mostly consist of resedimented slope deposits, produced by sliding of sediments, rich in lime mud, accumulated along the slope and low-angle proximal basin, whose instability (likely enhanced by seismic activity related to the Norian extensional tectonics) produced most of the recognised facies types. The two-step depositional processes as well as the facies associations and bed types clearly indicate a different behaviour (in terms of prevailing depositional processes and facies associations) of the studied resedimented limestone with respect to siliciclastic deposits. The distribution of facies and the detailed analyses of bed types, recording the distribution of depositional processes at basinal scale, provide a tool for the interpretation of basin morphology, from the study of stratigraphic logs, that can be applied both to outcrop and to subsurface successions." @default.
• W4213431388 created "2022-02-25" @default.
• W4213431388 creator A5052837329 @default.
• W4213431388 creator A5077375879 @default.
• W4213431388 date "2022-04-01" @default.
• W4213431388 modified "2023-09-24" @default.
• W4213431388 title "Resedimented limestones in fault-controlled basins (Zorzino Limestone, Southern Alps, Norian, Italy): Facies types and depositional model" @default.
• W4213431388 cites W1570489493 @default.
• W4213431388 cites W1934469433 @default.
• W4213431388 cites W1970729026 @default.
• W4213431388 cites W1970940931 @default.
• W4213431388 cites W1975478509 @default.
• W4213431388 cites W1983736505 @default.
• W4213431388 cites W1985238424 @default.
• W4213431388 cites W1992444350 @default.
• W4213431388 cites W1995863343 @default.
• W4213431388 cites W2018999844 @default.
• W4213431388 cites W2023318526 @default.
• W4213431388 cites W2046091863 @default.
• W4213431388 cites W2047378475 @default.
• W4213431388 cites W2047527622 @default.
• W4213431388 cites W2051297692 @default.
• W4213431388 cites W2053518653 @default.
• W4213431388 cites W2058366022 @default.
• W4213431388 cites W2059923107 @default.
• W4213431388 cites W2061513052 @default.
• W4213431388 cites W2067927835 @default.
• W4213431388 cites W2069724073 @default.
• W4213431388 cites W2081790539 @default.
• W4213431388 cites W2089598085 @default.
• W4213431388 cites W2098479229 @default.
• W4213431388 cites W2114987349 @default.
• W4213431388 cites W2120162798 @default.
• W4213431388 cites W2126274779 @default.
• W4213431388 cites W2170427367 @default.
• W4213431388 cites W2410021807 @default.
• W4213431388 cites W2743449741 @default.
• W4213431388 cites W2904879116 @default.
• W4213431388 cites W3000131874 @default.
• W4213431388 cites W3033084766 @default.
• W4213431388 cites W4241764248 @default.
• W4213431388 cites W86893661 @default.
• W4213431388 doi "https://doi.org/10.1016/j.sedgeo.2022.106106" @default.
• W4213431388 hasPublicationYear "2022" @default.
• W4213431388 type Work @default.
• W4213431388 citedByCount "2" @default.
• W4213431388 countsByYear W42134313882022 @default.
• W4213431388 crossrefType "journal-article" @default.
• W4213431388 hasAuthorship W4213431388A5052837329 @default.
• W4213431388 hasAuthorship W4213431388A5077375879 @default.
• W4213431388 hasConcept C106804226 @default.
• W4213431388 hasConcept C109007969 @default.
• W4213431388 hasConcept C114793014 @default.
• W4213431388 hasConcept C126753816 @default.
• W4213431388 hasConcept C127313418 @default.
• W4213431388 hasConcept C138170599 @default.
• W4213431388 hasConcept C146588470 @default.
• W4213431388 hasConcept C151730666 @default.
• W4213431388 hasConcept C17409809 @default.
• W4213431388 hasConcept C175551986 @default.
• W4213431388 hasConcept C5900021 @default.
• W4213431388 hasConcept C6494504 @default.
• W4213431388 hasConceptScore W4213431388C106804226 @default.
• W4213431388 hasConceptScore W4213431388C109007969 @default.
• W4213431388 hasConceptScore W4213431388C114793014 @default.
• W4213431388 hasConceptScore W4213431388C126753816 @default.
• W4213431388 hasConceptScore W4213431388C127313418 @default.
• W4213431388 hasConceptScore W4213431388C138170599 @default.
• W4213431388 hasConceptScore W4213431388C146588470 @default.
• W4213431388 hasConceptScore W4213431388C151730666 @default.
• W4213431388 hasConceptScore W4213431388C17409809 @default.
• W4213431388 hasConceptScore W4213431388C175551986 @default.
• W4213431388 hasConceptScore W4213431388C5900021 @default.
• W4213431388 hasConceptScore W4213431388C6494504 @default.
• W4213431388 hasLocation W42134313881 @default.
• W4213431388 hasOpenAccess W4213431388 @default.
• W4213431388 hasPrimaryLocation W42134313881 @default.
• W4213431388 hasRelatedWork W1958275154 @default.
• W4213431388 hasRelatedWork W1981062320 @default.
• W4213431388 hasRelatedWork W1991485717 @default.
• W4213431388 hasRelatedWork W2045809124 @default.
• W4213431388 hasRelatedWork W2349549624 @default.
• W4213431388 hasRelatedWork W2351927365 @default.
• W4213431388 hasRelatedWork W2355280957 @default.
• W4213431388 hasRelatedWork W2368842717 @default.
• W4213431388 hasRelatedWork W2372786881 @default.
• W4213431388 hasRelatedWork W2595561582 @default.
• W4213431388 hasVolume "431" @default.
• W4213431388 isParatext "false" @default.
• W4213431388 isRetracted "false" @default.
• W4213431388 workType "article" @default.