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dc.contributor.authorD'Elía, Leandroes_ES
dc.contributor.authorMartí Molist, Joanes_ES
dc.contributor.authorMuravchik, Martínes_ES
dc.contributor.authorBilmes, Andréses_ES
dc.contributor.authorFranzese, Juan R.es_ES
dc.date.accessioned2017-01-09T10:14:41Z-
dc.date.available2017-01-09T10:14:41Z-
dc.date.issued2016-11-
dc.identifier.citationBasin Research: 1-25 (2016)es_ES
dc.identifier.issn0950-091X-
dc.identifier.urihttp://hdl.handle.net/10261/142259-
dc.description.abstractThe analysis of volcano-sedimentary infill in sedimentary basins constitutes a challenge for basin analysis and hydrocarbon exploration worldwide. In order to understand the contribution of volcanism to the sedimentary record in rift basins, we study the Jurassic effusive-explosive volcanic infill of an inverted extensional depocentre at the Neuquén Basin, Argentina. A cause and effect model that evaluates the relationship between volcanism and sedimentation was devised to develop a conceptual model for the tectono-stratigraphic evolution of this volcanic rift basin. We show how the variations in the volcanism, coupled with the activity of extensional faults, determined the types of volcanic edifices (i.e., composite volcanoes, graben-calderas, and lava fields). Volcanic edifices controlled the stacking patterns of the volcanic units as well as sedimentary systems. The landform of the volcanic edifices, as well as the styles and scales of the eruptions governed the sedimentary input to the basin, setting the main variables of the sedimentary systems, such as provenance, grain size, transport and deposition and geometry. As a result, the contrasting volcaniclastic input, from higher volcaniclastic input to lower volcaniclastic input, associated with different subsidence patterns, determined the high-resolution syn-rift infill patterns of the extensional depocentre. The cause and effect model presented in this study isolates the variables of the volcanic environments that control the sedimentary scenarios. We suggest that, by adjusting the first order input parameters of the model, these cause and effect scenarios could be adapted to similar rift basins, in order to establish predictive facies models with stratigraphic controls, and the impact of volcanism on their stratigraphic records. © 2016 John Wiley & Sons Ltd, European Association of Geoscientists & Engineers and International Association of Sedimentologists.es_ES
dc.description.sponsorshipThis research was funded by the Agencia Nacional de Promoción Científica y Tecnológica, BID-PICT 2013-1888, the Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET, Argentina), the Consejo Superior de Investigaciones Científicas (CSIC, Spain), and a MICINN grant CGL2010-22022-C02-02.es_ES
dc.language.isoenges_ES
dc.publisherWiley-Blackwelles_ES
dc.rightsclosedAccesses_ES
dc.titleImpact of volcanism on the sedimentary record of the Neuquén rift basin, Argentina: Towards a cause and effect modeles_ES
dc.typeartículoes_ES
dc.identifier.doi10.1111/bre.12222-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://dx.doi.org/10.1111/bre.12222es_ES
dc.identifier.e-issn1365-2117-
dc.contributor.funderAgencia Nacional de Promoción Científica y Tecnológica (Argentina)es_ES
dc.contributor.funderConsejo Nacional de Investigaciones Científicas y Técnicas (Argentina)es_ES
dc.contributor.funderMinisterio de Ciencia e Innovación (España)es_ES
dc.relation.csices_ES
oprm.item.hasRevisionno ko 0 false*
dc.identifier.funderhttp://dx.doi.org/10.13039/501100003074es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/501100002923es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/501100004837es_ES
dc.type.coarhttp://purl.org/coar/resource_type/c_6501es_ES
item.openairetypeartículo-
item.fulltextNo Fulltext-
item.grantfulltextnone-
item.languageiso639-1en-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.cerifentitytypePublications-
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