A Prodeltaic System Controlled By Hyperpycnal Flows And Storm Waves: Reinterpretation Of The Punta Negra Formation (lower-middle Devonian, Argentine Precordillera)

dc.creatorDe Luca P.H.V.
dc.creatorBasilici G.
dc.date2013
dc.date2015-06-25T19:11:18Z
dc.date2015-11-26T15:08:47Z
dc.date2015-06-25T19:11:18Z
dc.date2015-11-26T15:08:47Z
dc.date.accessioned2018-03-28T22:19:06Z
dc.date.available2018-03-28T22:19:06Z
dc.identifier
dc.identifierBrazilian Journal Of Geology. , v. 43, n. 4, p. 673 - 694, 2013.
dc.identifier23174889
dc.identifier10.5327/Z2317-48892013000400008
dc.identifierhttp://www.scopus.com/inward/record.url?eid=2-s2.0-84892656495&partnerID=40&md5=900eca93139ff6c9f03dbf06a2d0e799
dc.identifierhttp://www.repositorio.unicamp.br/handle/REPOSIP/88632
dc.identifierhttp://repositorio.unicamp.br/jspui/handle/REPOSIP/88632
dc.identifier2-s2.0-84892656495
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/1257725
dc.descriptionThe Punta Negra Formation (FPN) constitutes a Lower-Middle Devonian sandstone unit located in the Argentine Precordillera. Based on detailed facies and ichnological analyses, this unit, which had been previously interpreted as a deep-water system, has been reinterpreted in this study as a prodelta system, in which the distribution and sedimentation of the clastic deposits were controlled by hyperpycnal flows associated with storms. Five lithofacies attest the deposition by unidirectional hyperpycnal flows combined with storm-generated oscillatory flows. Fossil traces testify variable energetic conditions of the depositional system with the colonization of opportunistic organisms immediately after the deposition of high energy combined flows and the colonization of more specialized organisms during the long low-energy periods. Three architectural elements, deposited from coastline to offshore, have been recognized: 1) Channelized sandstone, composed of the thickest and coarsest sandstone beds and interpreted as the proximal portion deposited close to the mouth of the distributaries of the delta system; 2) Tabular sandstone, which are composed of combined and oscillatory flow deposits with lesser thickness, grain size and spacing of the undulated bed forms; 3) Tabular sandstone interbedded to mudstone, which represents the most distal architectural element and is composed of thin sandstone and thicker mudstone strata, deposited by low-energy combined flows.
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dc.languageen
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dc.relationBrazilian Journal of Geology
dc.rightsaberto
dc.sourceScopus
dc.titleA Prodeltaic System Controlled By Hyperpycnal Flows And Storm Waves: Reinterpretation Of The Punta Negra Formation (lower-middle Devonian, Argentine Precordillera)
dc.typeArtículos de revistas


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