FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2034774332> ?p ?o ?g. }

• W2034774332 endingPage "27" @default.
• W2034774332 startingPage "5" @default.
• W2034774332 abstract "We have reconstructed the depositional environment of the gypsum-carbonate-shale sequence that comprises the Upper Permian Bellerophon Formation of the southeastern Alps in northern Italy. This formation, which reaches a maximum thickness of 600 m, is roughly divided into two facies: (a) a lower dolomite-gypsum facies, and (2) an upper micritic-skeletal limestone facies. It directly overlies, with transitional contact, a thick red-bed sequence (alluvial fanglomerates, fluviatile sandstones and flood-plain siltstones) and is sharply overlain by Lower Triassic calcarenites (oolites, grapestones, pellets, flat-pebble conglomerates). The lower evaporite facies rocks are found in well-defined cycles, each of which, from bottom to top, consists of (A) thin-bedded, worm-burrowed, vuggy ‘earthy’ micritic dolomite, (B) massive to poorly laminated dark grey to black sandy dolomite carrying isolated gypsum nodules, (C) layered (thin-bedded) nodular gypsum (commonly with ‘enterolithic’ folds) with fragmented partings of dolomite, and (D) massive ‘chicken-wire’ nodular gypsum. At Passo di Valles, just east of Predazzo, and 50 km from the basin margin, we measured forty-six consecutive complete cycles, with an average thickness of 3 m per cycle. We interpret the cyclic sequence as having been deposited in a prograding shallow lagoon—sabkha complex. The worm-burrowed ‘earthy’ dolomite mud accumulated in a shallow hypersaline subtidal lagoon. The black sandy dolomite was an ‘intertidal’ sand-flat devoid of algal mats and constantly churned by burrowers (likely crustaceans). As the shoreline prograded lagoonward evaporative concentration of the groundwater induced diagenetic growth of anhydrite nodules (now gypsum) within the porous sandy dolomite. The layered nodular and ‘chicken-wire’ gypsum of the cycle cap is an extreme product of such displacive intra-sediment growth of anhydrite (now gypsum) above the water table of a completely exposed sabkha, such as is found in the Persian Gulf today. We have observed the same cyclically arranged lithologies in two other evaporite sequences in Italy: the Triassic Raibl Formation of the Southern Alps and the Upper Triassic Burano Formation of the central Apennines. We suggest that this mode of deposition is likely a very common one for at least the early stages of marine evaporite accumulation." @default.
• W2034774332 created "2016-06-24" @default.
• W2034774332 creator A5013521433 @default.
• W2034774332 creator A5090906288 @default.
• W2034774332 date "1973-02-01" @default.
• W2034774332 modified "2023-10-18" @default.
• W2034774332 title "Depositional theme of a marginal marine evaporite" @default.
• W2034774332 cites W1967903325 @default.
• W2034774332 cites W1975282879 @default.
• W2034774332 cites W1977379643 @default.
• W2034774332 cites W1999772449 @default.
• W2034774332 cites W2008540853 @default.
• W2034774332 cites W2009941242 @default.
• W2034774332 cites W2012502690 @default.
• W2034774332 cites W2026853760 @default.
• W2034774332 cites W2043833070 @default.
• W2034774332 cites W2059752760 @default.
• W2034774332 cites W2091488432 @default.
• W2034774332 cites W2097133632 @default.
• W2034774332 cites W2108054309 @default.
• W2034774332 cites W2139355154 @default.
• W2034774332 cites W2167087774 @default.
• W2034774332 cites W4237617707 @default.
• W2034774332 cites W4255115523 @default.
• W2034774332 cites W619994375 @default.
• W2034774332 doi "https://doi.org/10.1111/j.1365-3091.1973.tb01604.x" @default.
• W2034774332 hasPublicationYear "1973" @default.
• W2034774332 type Work @default.
• W2034774332 sameAs 2034774332 @default.
• W2034774332 citedByCount "58" @default.
• W2034774332 countsByYear W20347743322012 @default.
• W2034774332 countsByYear W20347743322013 @default.
• W2034774332 countsByYear W20347743322014 @default.
• W2034774332 countsByYear W20347743322015 @default.
• W2034774332 countsByYear W20347743322017 @default.
• W2034774332 countsByYear W20347743322018 @default.
• W2034774332 countsByYear W20347743322019 @default.
• W2034774332 countsByYear W20347743322021 @default.
• W2034774332 countsByYear W20347743322022 @default.
• W2034774332 countsByYear W20347743322023 @default.
• W2034774332 crossrefType "journal-article" @default.
• W2034774332 hasAuthorship W2034774332A5013521433 @default.
• W2034774332 hasAuthorship W2034774332A5090906288 @default.
• W2034774332 hasConcept C109007969 @default.
• W2034774332 hasConcept C126753816 @default.
• W2034774332 hasConcept C127313418 @default.
• W2034774332 hasConcept C130452526 @default.
• W2034774332 hasConcept C146588470 @default.
• W2034774332 hasConcept C151730666 @default.
• W2034774332 hasConcept C17409809 @default.
• W2034774332 hasConcept C186660238 @default.
• W2034774332 hasConcept C191897082 @default.
• W2034774332 hasConcept C192562407 @default.
• W2034774332 hasConcept C2776044767 @default.
• W2034774332 hasConcept C2779229104 @default.
• W2034774332 hasConcept C2780181037 @default.
• W2034774332 hasConcept C2780659211 @default.
• W2034774332 hasConcept C34221334 @default.
• W2034774332 hasConcept C6494504 @default.
• W2034774332 hasConcept C85124164 @default.
• W2034774332 hasConceptScore W2034774332C109007969 @default.
• W2034774332 hasConceptScore W2034774332C126753816 @default.
• W2034774332 hasConceptScore W2034774332C127313418 @default.
• W2034774332 hasConceptScore W2034774332C130452526 @default.
• W2034774332 hasConceptScore W2034774332C146588470 @default.
• W2034774332 hasConceptScore W2034774332C151730666 @default.
• W2034774332 hasConceptScore W2034774332C17409809 @default.
• W2034774332 hasConceptScore W2034774332C186660238 @default.
• W2034774332 hasConceptScore W2034774332C191897082 @default.
• W2034774332 hasConceptScore W2034774332C192562407 @default.
• W2034774332 hasConceptScore W2034774332C2776044767 @default.
• W2034774332 hasConceptScore W2034774332C2779229104 @default.
• W2034774332 hasConceptScore W2034774332C2780181037 @default.
• W2034774332 hasConceptScore W2034774332C2780659211 @default.
• W2034774332 hasConceptScore W2034774332C34221334 @default.
• W2034774332 hasConceptScore W2034774332C6494504 @default.
• W2034774332 hasConceptScore W2034774332C85124164 @default.
• W2034774332 hasIssue "1" @default.
• W2034774332 hasLocation W20347743321 @default.
• W2034774332 hasOpenAccess W2034774332 @default.
• W2034774332 hasPrimaryLocation W20347743321 @default.
• W2034774332 hasRelatedWork W1823511438 @default.
• W2034774332 hasRelatedWork W2012676659 @default.
• W2034774332 hasRelatedWork W2023004289 @default.
• W2034774332 hasRelatedWork W2044225683 @default.
• W2034774332 hasRelatedWork W2056797263 @default.
• W2034774332 hasRelatedWork W2057052829 @default.
• W2034774332 hasRelatedWork W2112218706 @default.
• W2034774332 hasRelatedWork W2465953013 @default.
• W2034774332 hasRelatedWork W2915361100 @default.
• W2034774332 hasRelatedWork W3171651726 @default.
• W2034774332 hasVolume "20" @default.
• W2034774332 isParatext "false" @default.
• W2034774332 isRetracted "false" @default.
• W2034774332 magId "2034774332" @default.
• W2034774332 workType "article" @default.