FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3100700579> ?p ?o ?g. }

• W3100700579 endingPage "110109" @default.
• W3100700579 startingPage "110109" @default.
• W3100700579 abstract "Thick (>100 m-thick), highly bioturbated storm-influenced shallow-marine deposits are not frequent in the stratigraphic record, but they tend to be common in aggradational to retrogradational successions. Individual storm-event beds have typically low preservation potential in these successions, yet depositional settings are characterized on the basis of storms processes. Here we present a sedimentological study of a thick, bioturbated exhumed succession deposited during the early post-rift stage of the Neuquén Basin (Argentina) and compare its stratigraphic record with examples worldwide, in order to discuss the potential factors controlling the total overprint of storm-event beds during several million years. The Bardas Blancas Formation being 170–220 m thick in the study area is dominated by muddy sandstones and sandy mudstones, and it also includes subordinate proportions of clean sandstones and pure mudstones, collectively representing different environments of a storm-influenced shoreface-offshore system. The offshore transition and proximal offshore strata invariably comprise intensely bioturbated deposits, with only a few preserved HCS-sandstone beds. The unit shows for most of its thickness a long-term aggradational pattern spanning 7–10 Myr and is associated with low riverine influence. By combining the observations and interpretations of the Bardas Blancas Formation with other subsurface and exhumed intensely bioturbated, shallow-marine successions, we dispute the general assumption that these are associated with low frequency or low magnitude of storms. Alternatively, we argue that the long-lived efficiency of benthic fauna on overprinting most if not all the storm-event beds that reached the offshore-transition sector, results from the combination of several factors: deposition in relatively confined marine depocentres, persistent low riverine influence, and long-term aggradational stacking pattern. As these conditions can develop in a variety of basin styles, such as rift, early post-rift, and foreland settings, the recognition of thick, bioturbated successions as the ones discussed here can be used to infer more realistic constrains for depositional models and better predict facies distribution in such storm-influenced systems." @default.
• W3100700579 created "2020-11-23" @default.
• W3100700579 creator A5007266305 @default.
• W3100700579 creator A5010090718 @default.
• W3100700579 creator A5022650867 @default.
• W3100700579 creator A5042440836 @default.
• W3100700579 creator A5048954768 @default.
• W3100700579 date "2021-01-01" @default.
• W3100700579 modified "2023-10-10" @default.
• W3100700579 title "Architecture and controls of thick, intensely bioturbated, storm-influenced shallow-marine successions: An example from the Jurassic Neuquén Basin (Argentina)" @default.
• W3100700579 cites W1538456952 @default.
• W3100700579 cites W1697498229 @default.
• W3100700579 cites W1963886391 @default.
• W3100700579 cites W1968071575 @default.
• W3100700579 cites W1971103475 @default.
• W3100700579 cites W1984110690 @default.
• W3100700579 cites W2002011430 @default.
• W3100700579 cites W2017168185 @default.
• W3100700579 cites W2044778400 @default.
• W3100700579 cites W2045173275 @default.
• W3100700579 cites W2045231061 @default.
• W3100700579 cites W2047736471 @default.
• W3100700579 cites W2052639207 @default.
• W3100700579 cites W2074677640 @default.
• W3100700579 cites W2080547192 @default.
• W3100700579 cites W2082412673 @default.
• W3100700579 cites W2088381531 @default.
• W3100700579 cites W2103558226 @default.
• W3100700579 cites W2105107902 @default.
• W3100700579 cites W2116188466 @default.
• W3100700579 cites W2129479037 @default.
• W3100700579 cites W2136339718 @default.
• W3100700579 cites W2138480328 @default.
• W3100700579 cites W2156022682 @default.
• W3100700579 cites W2157891449 @default.
• W3100700579 cites W2337474080 @default.
• W3100700579 cites W2353254855 @default.
• W3100700579 cites W2767274412 @default.
• W3100700579 cites W2772946888 @default.
• W3100700579 cites W2774875355 @default.
• W3100700579 cites W3017920245 @default.
• W3100700579 doi "https://doi.org/10.1016/j.palaeo.2020.110109" @default.
• W3100700579 hasPublicationYear "2021" @default.
• W3100700579 type Work @default.
• W3100700579 sameAs 3100700579 @default.
• W3100700579 citedByCount "3" @default.
• W3100700579 countsByYear W31007005792021 @default.
• W3100700579 countsByYear W31007005792022 @default.
• W3100700579 countsByYear W31007005792023 @default.
• W3100700579 crossrefType "journal-article" @default.
• W3100700579 hasAuthorship W3100700579A5007266305 @default.
• W3100700579 hasAuthorship W3100700579A5010090718 @default.
• W3100700579 hasAuthorship W3100700579A5022650867 @default.
• W3100700579 hasAuthorship W3100700579A5042440836 @default.
• W3100700579 hasAuthorship W3100700579A5048954768 @default.
• W3100700579 hasBestOaLocation W31007005792 @default.
• W3100700579 hasConcept C105306849 @default.
• W3100700579 hasConcept C109007969 @default.
• W3100700579 hasConcept C111368507 @default.
• W3100700579 hasConcept C112959462 @default.
• W3100700579 hasConcept C126753816 @default.
• W3100700579 hasConcept C127313418 @default.
• W3100700579 hasConcept C130452526 @default.
• W3100700579 hasConcept C142614818 @default.
• W3100700579 hasConcept C151730666 @default.
• W3100700579 hasConcept C16156107 @default.
• W3100700579 hasConcept C162284963 @default.
• W3100700579 hasConcept C2778660078 @default.
• W3100700579 hasConcept C2816523 @default.
• W3100700579 hasConcept C65589250 @default.
• W3100700579 hasConcept C77928131 @default.
• W3100700579 hasConceptScore W3100700579C105306849 @default.
• W3100700579 hasConceptScore W3100700579C109007969 @default.
• W3100700579 hasConceptScore W3100700579C111368507 @default.
• W3100700579 hasConceptScore W3100700579C112959462 @default.
• W3100700579 hasConceptScore W3100700579C126753816 @default.
• W3100700579 hasConceptScore W3100700579C127313418 @default.
• W3100700579 hasConceptScore W3100700579C130452526 @default.
• W3100700579 hasConceptScore W3100700579C142614818 @default.
• W3100700579 hasConceptScore W3100700579C151730666 @default.
• W3100700579 hasConceptScore W3100700579C16156107 @default.
• W3100700579 hasConceptScore W3100700579C162284963 @default.
• W3100700579 hasConceptScore W3100700579C2778660078 @default.
• W3100700579 hasConceptScore W3100700579C2816523 @default.
• W3100700579 hasConceptScore W3100700579C65589250 @default.
• W3100700579 hasConceptScore W3100700579C77928131 @default.
• W3100700579 hasFunder F4320317044 @default.
• W3100700579 hasFunder F4320321594 @default.
• W3100700579 hasFunder F4320322227 @default.
• W3100700579 hasFunder F4320323260 @default.
• W3100700579 hasLocation W31007005791 @default.
• W3100700579 hasLocation W31007005792 @default.
• W3100700579 hasLocation W31007005793 @default.
• W3100700579 hasLocation W31007005794 @default.
• W3100700579 hasLocation W31007005795 @default.
• W3100700579 hasOpenAccess W3100700579 @default.
• W3100700579 hasPrimaryLocation W31007005791 @default.
• W3100700579 hasRelatedWork W193840547 @default.

• next