dc.creatorBallen O.A.R.
dc.creatorGoes A.M.
dc.creatorDe Assis Negri F.
dc.creatorMaziviero M.V.
dc.creatorDo Santos Teixeira V.Z.
dc.date2013
dc.date2015-06-25T19:11:16Z
dc.date2015-11-26T15:09:02Z
dc.date2015-06-25T19:11:16Z
dc.date2015-11-26T15:09:02Z
dc.date.accessioned2018-03-28T22:19:15Z
dc.date.available2018-03-28T22:19:15Z
dc.identifier
dc.identifierBrazilian Journal Of Geology. , v. 43, n. 4, p. 695 - 710, 2013.
dc.identifier23174889
dc.identifier10.5327/Z2317-48892013000400009
dc.identifierhttp://www.scopus.com/inward/record.url?eid=2-s2.0-84892635885&partnerID=40&md5=fb4d0f9d57e47b5a5c80db8df9d88264
dc.identifierhttp://www.repositorio.unicamp.br/handle/REPOSIP/88631
dc.identifierhttp://repositorio.unicamp.br/jspui/handle/REPOSIP/88631
dc.identifier2-s2.0-84892635885
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/1257739
dc.descriptionPrior to the tectonic events related to the opening of the Central Atlantic, the Mosquito Formation of Jurassic age in the Parnaiba Sedimentary Basin was deposited as a succession of interbedded basaltic flows and sedimentary packets. The sedimentary successions deposits accumulated in topographic depressions with erosional contacts at both their base and top. Their contacts with the basalts are marked by eolian supersurfaces. The thickest intertrapp unit in the formation, the Macap̀ Member, found in the Mosquito river valley, is made up of sandstones comprising three facies associations: 1) eolian dune fields with interdune pond deposits, 2) sand sheets with ephemeral fluvial deposits and 3) siliciclastic sabkha. Relative water level, which controlled sediment availability and the accumulation surface and varied as a function of climate and probably subsidence rate, was the most important factor affecting intertrapp sedimentation in the Mosquito Formation.
dc.description43
dc.description4
dc.description695
dc.description710
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dc.languagept
dc.publisher
dc.relationBrazilian Journal of Geology
dc.rightsaberto
dc.sourceScopus
dc.titleAeolian Wet System In The Sedimentary Intertraps Successions Of Mosquito Formation, Jurassic Of The Parnaiba Province, Brazil [sistema Eólico úmido Nas Sucessões Sedimentares Interderrames Da Formação Mosquito, Jur̀ssico Da Província Parnaíba, Brasil]
dc.typeArtículos de revistas


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