Matches in SemOpenAlex for { <https://semopenalex.org/work/W2810379070> ?p ?o ?g. }
- W2810379070 endingPage "2071" @default.
- W2810379070 startingPage "2049" @default.
- W2810379070 abstract "The Ipubi Formation represents the Aptian-Albian siliciclastic-evaporitic succession of Araripe Basin, NE Brazil. This succession comprises siliciclastic rocks (bituminous shales and claystones) and evaporites (gypsum and secondary anhydrite) and represents part of the lacustrine-shallow marine post-rift phase I. This study used sequence stratigraphy concepts to define the relations between changes in the relative lake level and the formation of Ipubi deposits. Results show that the organic-rich shales of the Ipubi Formation formed during a transgressive pulse that covered large areas of the proximal domains. These deposits overlie a regional unconformity that marks the end of the deposition of the underlying Crato Formation. A High Stand stage that followed the transgression influenced the formation of evaporitic deposits. Climate conditions played a major role in influencing the triggering and stopping of evaporite deposition. Thus, a new relative lake level fall event caused the exposure of the Ipubi Formation deposits, and created another regional subaerial unconformity accompanied by widespread karstification of evaporite beds. A posterior transgression caused the deposition of siliciclastic rocks of the Romualdo Formation over the Ipubi Formation strata, and also promoted a new event of karstification of the Ipubi upper evaporite beds." @default.
- W2810379070 created "2018-07-10" @default.
- W2810379070 creator A5007958856 @default.
- W2810379070 creator A5026353952 @default.
- W2810379070 creator A5040297584 @default.
- W2810379070 creator A5057186651 @default.
- W2810379070 creator A5074284116 @default.
- W2810379070 creator A5074930223 @default.
- W2810379070 creator A5085341544 @default.
- W2810379070 creator A5089286529 @default.
- W2810379070 date "2018-08-01" @default.
- W2810379070 modified "2023-10-14" @default.
- W2810379070 title "Stratigraphic Relations of the Ipubi Formation: Siliciclastic-Evaporitic Succession of the Araripe Basin" @default.
- W2810379070 cites W1982258379 @default.
- W2810379070 cites W1989397756 @default.
- W2810379070 cites W1993960210 @default.
- W2810379070 cites W2013015520 @default.
- W2810379070 cites W2013403815 @default.
- W2810379070 cites W2015296778 @default.
- W2810379070 cites W2023515382 @default.
- W2810379070 cites W2024361351 @default.
- W2810379070 cites W2032123209 @default.
- W2810379070 cites W2047823257 @default.
- W2810379070 cites W2050440902 @default.
- W2810379070 cites W2059794687 @default.
- W2810379070 cites W2075689805 @default.
- W2810379070 cites W2087090612 @default.
- W2810379070 cites W2093879665 @default.
- W2810379070 cites W2098068539 @default.
- W2810379070 cites W2108431640 @default.
- W2810379070 cites W2129301875 @default.
- W2810379070 cites W2139892557 @default.
- W2810379070 cites W2149736100 @default.
- W2810379070 cites W2173623002 @default.
- W2810379070 cites W2201676221 @default.
- W2810379070 cites W2403014497 @default.
- W2810379070 cites W2413812975 @default.
- W2810379070 cites W2415516716 @default.
- W2810379070 cites W2516162423 @default.
- W2810379070 cites W2528025970 @default.
- W2810379070 cites W2563448770 @default.
- W2810379070 cites W2581782420 @default.
- W2810379070 cites W2605387680 @default.
- W2810379070 cites W2973691113 @default.
- W2810379070 doi "https://doi.org/10.1590/0001-3765201820170526" @default.
- W2810379070 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/29947671" @default.
- W2810379070 hasPublicationYear "2018" @default.
- W2810379070 type Work @default.
- W2810379070 sameAs 2810379070 @default.
- W2810379070 citedByCount "14" @default.
- W2810379070 countsByYear W28103790702020 @default.
- W2810379070 countsByYear W28103790702021 @default.
- W2810379070 countsByYear W28103790702022 @default.
- W2810379070 countsByYear W28103790702023 @default.
- W2810379070 crossrefType "journal-article" @default.
- W2810379070 hasAuthorship W2810379070A5007958856 @default.
- W2810379070 hasAuthorship W2810379070A5026353952 @default.
- W2810379070 hasAuthorship W2810379070A5040297584 @default.
- W2810379070 hasAuthorship W2810379070A5057186651 @default.
- W2810379070 hasAuthorship W2810379070A5074284116 @default.
- W2810379070 hasAuthorship W2810379070A5074930223 @default.
- W2810379070 hasAuthorship W2810379070A5085341544 @default.
- W2810379070 hasAuthorship W2810379070A5089286529 @default.
- W2810379070 hasBestOaLocation W28103790701 @default.
- W2810379070 hasConcept C109007969 @default.
- W2810379070 hasConcept C126753816 @default.
- W2810379070 hasConcept C127313418 @default.
- W2810379070 hasConcept C150117547 @default.
- W2810379070 hasConcept C151730666 @default.
- W2810379070 hasConcept C17409809 @default.
- W2810379070 hasConcept C18903297 @default.
- W2810379070 hasConcept C191735495 @default.
- W2810379070 hasConcept C2776044767 @default.
- W2810379070 hasConcept C2779229104 @default.
- W2810379070 hasConcept C34221334 @default.
- W2810379070 hasConcept C6494504 @default.
- W2810379070 hasConcept C77271252 @default.
- W2810379070 hasConcept C84983702 @default.
- W2810379070 hasConcept C86803240 @default.
- W2810379070 hasConcept C93257316 @default.
- W2810379070 hasConceptScore W2810379070C109007969 @default.
- W2810379070 hasConceptScore W2810379070C126753816 @default.
- W2810379070 hasConceptScore W2810379070C127313418 @default.
- W2810379070 hasConceptScore W2810379070C150117547 @default.
- W2810379070 hasConceptScore W2810379070C151730666 @default.
- W2810379070 hasConceptScore W2810379070C17409809 @default.
- W2810379070 hasConceptScore W2810379070C18903297 @default.
- W2810379070 hasConceptScore W2810379070C191735495 @default.
- W2810379070 hasConceptScore W2810379070C2776044767 @default.
- W2810379070 hasConceptScore W2810379070C2779229104 @default.
- W2810379070 hasConceptScore W2810379070C34221334 @default.
- W2810379070 hasConceptScore W2810379070C6494504 @default.
- W2810379070 hasConceptScore W2810379070C77271252 @default.
- W2810379070 hasConceptScore W2810379070C84983702 @default.
- W2810379070 hasConceptScore W2810379070C86803240 @default.
- W2810379070 hasConceptScore W2810379070C93257316 @default.
- W2810379070 hasIssue "2 suppl 1" @default.
- W2810379070 hasLocation W28103790701 @default.