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dc.provenanceCONICET-
dc.creatorMartín Chivelet, Javier-
dc.creatorPalma, Ricardo Manuel-
dc.creatorLópez Gómez, José-
dc.creatorKietzmann, Diego Alejandro-
dc.date2019-01-23T18:45:48Z-
dc.date2019-01-23T18:45:48Z-
dc.date2011-04-
dc.date2019-01-23T17:16:37Z-
dc.date.accessioned2019-04-29T15:44:50Z-
dc.date.available2019-04-29T15:44:50Z-
dc.date.issued2011-04-
dc.identifierMartín Chivelet, Javier; Palma, Ricardo Manuel; López Gómez, José; Kietzmann, Diego Alejandro; Earthquake-induced soft-sediment deformation structures in Upper Jurassic open-marine microbialites (Neuquén Basin, Argentina); Elsevier Science; Sedimentary Geology; 235; 3-4; 4-2011; 210-221-
dc.identifier0037-0738-
dc.identifierhttp://hdl.handle.net/11336/68470-
dc.identifierCONICET Digital-
dc.identifierCONICET-
dc.identifier.urihttp://rodna.bn.gov.ar:8080/jspui/handle/bnmm/300965-
dc.descriptionPenecontemporaneous decimetre-scale soft-sediment deformation structures are reported from the basal part of the Upper Jurassic-Lower Cretaceous Vaca Muerta Formation, in the Malargüe-Las Leñas area of the back-arc Neuquén Basin (Mendoza Province, Central Andes). The deformed interval (Amarillas bed) is only 0.3 to 0.9m thick but occurs in a wide area, larger than 1500km2. Its age, determined by ammonite biostratigraphy, is Early Tithonian.The soft-sediment deformation structures were generated in finely laminated, partially consolidated, organic-rich, carbonate microbialites that were deposited in open-marine, poorly oxygenated settings, apparently devoid of any significant slope. Those structures include boudins of different sizes and complexity, a variety of folds, normal (listric) dm-scale faults, sub-horizontal detachment surfaces and other features, which are part of several larger-scale, complex slump structures. Deformation was dominantly plastic but near to the ductile-brittle field transition.On the basis of the observed soft-deformation structures, their geographic distribution, their lateral homogeneity, and the geodynamic framework of the basin in which it was generated, the Amarillas bed can be tentatively attributed to a large, intermediate-depth earthquake that occurred within the plate that subducted beneath the Andean continental margin and the Neuquén back-arc basin.-
dc.descriptionFil: Martín Chivelet, Javier. Universidad Complutense de Madrid; España-
dc.descriptionFil: Palma, Ricardo Manuel. Universidad de Chile. Facultad de Ciencias Físicas y Matemáticas. Departamento de Geología; Chile. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina-
dc.descriptionFil: López Gómez, José. Universidad Complutense de Madrid; España-
dc.descriptionFil: Kietzmann, Diego Alejandro. Universidad de Chile. Facultad de Ciencias Físicas y Matemáticas. Departamento de Geología; Chile. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina-
dc.formatapplication/pdf-
dc.formatapplication/pdf-
dc.languageeng-
dc.publisherElsevier Science-
dc.relationinfo:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1016/j.sedgeo.2010.09.017-
dc.relationinfo:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0037073810002770-
dc.rightsinfo:eu-repo/semantics/restrictedAccess-
dc.rightshttps://creativecommons.org/licenses/by-nc-nd/2.5/ar/-
dc.sourcereponame:CONICET Digital (CONICET)-
dc.sourceinstname:Consejo Nacional de Investigaciones Científicas y Técnicas-
dc.sourceinstacron:CONICET-
dc.source.urihttp://hdl.handle.net/11336/68470-
dc.subjectANDES-
dc.subjectBACK-ARC BASIN-
dc.subjectCARBONATE ROCKS-
dc.subjectSEISMITES-
dc.subjectSOFT-SEDIMENT DEFORMATION-
dc.subjectTITHONIAN-
dc.subjectGeología-
dc.subjectCiencias de la Tierra y relacionadas con el Medio Ambiente-
dc.subjectCIENCIAS NATURALES Y EXACTAS-
dc.titleEarthquake-induced soft-sediment deformation structures in Upper Jurassic open-marine microbialites (Neuquén Basin, Argentina)-
dc.typeinfo:eu-repo/semantics/article-
dc.typeinfo:eu-repo/semantics/publishedVersion-
dc.typeinfo:ar-repo/semantics/articulo-
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