FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2024488818> ?p ?o ?g. }

• W2024488818 endingPage "116" @default.
• W2024488818 startingPage "97" @default.
• W2024488818 abstract "The Lower Cretaceous geological record of the intracratonic Paraná Basin in southern Brazil comprises a thick succession of aeolian sandstones and volcanic rocks. The intercalation between aeolian sandstone and volcanic floods allowed the preservation of distinct aeolian genetic units. Each genetic unit represents an accumulation episode, bounded by supersurfaces, that coincides with the base of lava flood events. The entire package can be subdivided into a Lower Genetic Unit, which corresponds to aeolian sandstones preserved below the initial lava flows (Botucatu Formation), and an upper set of genetic units, which comprises interlayered aeolian deposits and lava floods (Serra Geral Formation). The Lower Genetic Unit is up to 100 m thick. Its base is composed of ephemeral stream and aeolian sand sheet deposits that are overlain by cross-bedded sandstones whose origin is ascribed to simple, locally composite, crescentic and complex linear aeolian dunes. Aeolian accumulation of the lower unit was possible as a result of the existence of a wide topographic basin, which caused wind deceleration, and a large sand availability that promoted a positive net sediment flux. The Upper Genetic Units comprise isolated sand bodies that occur in two different styles: (1) thin lenses (<3 m thick) formed by aeolian sand sheets; and (2) thick sand lenses (3–15 m) comprising cross-bedded cosets generated by migration and climbing of simple to locally composite crescentic aeolian dunes. Accumulation of the aeolian strata was associated with wind deceleration within depressions on the irregular upper surface of the lava floods. The interruption of sedimentation in the Lower and Upper Genetic Units, and related development of supersurfaces, occurred as a result of widespread effusions of basaltic lava. Preservation of both wind-rippled topset deposits of the aeolian dunes and pahoehoe lava imprints indicates that lava floods covered active aeolian dunes and, hence, protected the aeolian deposits from erosion, thus preserving the genetic units." @default.
• W2024488818 created "2016-06-24" @default.
• W2024488818 creator A5000563253 @default.
• W2024488818 date "2002-02-01" @default.
• W2024488818 modified "2023-10-10" @default.
• W2024488818 title "Preservation of aeolian genetic units by lava flows in the Lower Cretaceous of the Paraná Basin, southern Brazil" @default.
• W2024488818 cites W1965801550 @default.
• W2024488818 cites W1972280618 @default.
• W2024488818 cites W1981434834 @default.
• W2024488818 cites W1985389344 @default.
• W2024488818 cites W1994334962 @default.
• W2024488818 cites W2011311463 @default.
• W2024488818 cites W2016272372 @default.
• W2024488818 cites W2018420184 @default.
• W2024488818 cites W2021808919 @default.
• W2024488818 cites W2023884785 @default.
• W2024488818 cites W2038171999 @default.
• W2024488818 cites W2047709627 @default.
• W2024488818 cites W2048722474 @default.
• W2024488818 cites W2067948719 @default.
• W2024488818 cites W2071548211 @default.
• W2024488818 cites W2075280574 @default.
• W2024488818 cites W2078876156 @default.
• W2024488818 cites W2087912598 @default.
• W2024488818 cites W2088427166 @default.
• W2024488818 cites W2092271616 @default.
• W2024488818 cites W2100766326 @default.
• W2024488818 cites W2101477926 @default.
• W2024488818 cites W2116238496 @default.
• W2024488818 cites W2119278745 @default.
• W2024488818 cites W2133884642 @default.
• W2024488818 cites W2227837164 @default.
• W2024488818 cites W2916759378 @default.
• W2024488818 cites W2972853859 @default.
• W2024488818 cites W3194083978 @default.
• W2024488818 cites W4230939369 @default.
• W2024488818 cites W991822163 @default.
• W2024488818 doi "https://doi.org/10.1046/j.1365-3091.2002.00434.x" @default.
• W2024488818 hasPublicationYear "2002" @default.
• W2024488818 type Work @default.
• W2024488818 sameAs 2024488818 @default.
• W2024488818 citedByCount "113" @default.
• W2024488818 countsByYear W20244888182012 @default.
• W2024488818 countsByYear W20244888182013 @default.
• W2024488818 countsByYear W20244888182014 @default.
• W2024488818 countsByYear W20244888182015 @default.
• W2024488818 countsByYear W20244888182016 @default.
• W2024488818 countsByYear W20244888182017 @default.
• W2024488818 countsByYear W20244888182018 @default.
• W2024488818 countsByYear W20244888182019 @default.
• W2024488818 countsByYear W20244888182020 @default.
• W2024488818 countsByYear W20244888182021 @default.
• W2024488818 countsByYear W20244888182022 @default.
• W2024488818 countsByYear W20244888182023 @default.
• W2024488818 crossrefType "journal-article" @default.
• W2024488818 hasAuthorship W2024488818A5000563253 @default.
• W2024488818 hasConcept C113754120 @default.
• W2024488818 hasConcept C114793014 @default.
• W2024488818 hasConcept C120806208 @default.
• W2024488818 hasConcept C12294951 @default.
• W2024488818 hasConcept C127313418 @default.
• W2024488818 hasConcept C151730666 @default.
• W2024488818 hasConcept C17409809 @default.
• W2024488818 hasConcept C180093795 @default.
• W2024488818 hasConceptScore W2024488818C113754120 @default.
• W2024488818 hasConceptScore W2024488818C114793014 @default.
• W2024488818 hasConceptScore W2024488818C120806208 @default.
• W2024488818 hasConceptScore W2024488818C12294951 @default.
• W2024488818 hasConceptScore W2024488818C127313418 @default.
• W2024488818 hasConceptScore W2024488818C151730666 @default.
• W2024488818 hasConceptScore W2024488818C17409809 @default.
• W2024488818 hasConceptScore W2024488818C180093795 @default.
• W2024488818 hasIssue "1" @default.
• W2024488818 hasLocation W20244888181 @default.
• W2024488818 hasOpenAccess W2024488818 @default.
• W2024488818 hasPrimaryLocation W20244888181 @default.
• W2024488818 hasRelatedWork W1596462920 @default.
• W2024488818 hasRelatedWork W1992776973 @default.
• W2024488818 hasRelatedWork W2000553602 @default.
• W2024488818 hasRelatedWork W2015231778 @default.
• W2024488818 hasRelatedWork W2027128207 @default.
• W2024488818 hasRelatedWork W2070192581 @default.
• W2024488818 hasRelatedWork W2165955656 @default.
• W2024488818 hasRelatedWork W2325222095 @default.
• W2024488818 hasRelatedWork W2922117034 @default.
• W2024488818 hasRelatedWork W3213701310 @default.
• W2024488818 hasVolume "49" @default.
• W2024488818 isParatext "false" @default.
• W2024488818 isRetracted "false" @default.
• W2024488818 magId "2024488818" @default.
• W2024488818 workType "article" @default.