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dc.contributor.authorGómez, Ricardo-
dc.contributor.authorTunik, Maisa Andrea-
dc.contributor.authorCasadio, SIlvio Alberto-
dc.date.accessioned2020-06-23T15:12:36Z-
dc.date.available2020-06-23T15:12:36Z-
dc.date.issued2020-
dc.identifier.citationGómez, Ricardo., Tunik, Maisa A., Casadío, Silvio A. (2020). Fluvial deposits as a record of the Late Cretaceous tectonic activity in southern Central Andes, Argentina. Servicio Nacional de Geología y Minería; Andean Geology; 47 (2); 256-274.es_ES
dc.identifier.issn0718-7106es_ES
dc.identifier.issn0718-7092es_ES
dc.identifier.urihttp://www.andeangeology.cl/index.php/revista1/article/view/V47n2-3218/pdf-
dc.identifier.urihttps://rid.unrn.edu.ar/jspui/handle/20.500.12049/5351-
dc.format.extentp. 256-274es_ES
dc.format.mediumimpresoes_ES
dc.format.mediumdigitales_ES
dc.language.isoenes_ES
dc.publisherServicio Nacional de Geología y Mineríaes_ES
dc.titleFluvial deposits of the Diamante Formation as a record of the Late Cretaceous tectonic activity in the Southern Central Andes, Mendoza, Argentinaes_ES
dc.typeArticuloes_ES
dc.rights.licensehttps://creativecommons.org/licenses/by-nc-sa/4.0/es_ES
dc.description.filiationFil: Gómez, Ricardo. Museo de Historia Natural de San Rafael. Mendoza, Argentinaes_ES
dc.description.filiationFil: Tunik, Maisa A. Universidad Nacional de Río Negro. Instituto de Investigaciones en Paleobiología y Geología. Río Negro, Argentina.es_ES
dc.description.filiationFil: Casadio, Silvio A. Universidad Nacional de Río Negro. Instituto de Investigaciones en Paleobiología y Geología. Río Negro, Argentina.es_ES
dc.description.filiationFil: Gómez, Ricardo. Universidad Nacional de Río Negro. Instituto de Investigaciones en Paleobiología y Geología. Río Negro, Argentina.es_ES
dc.subject.keywordNeuquén Basines_ES
dc.subject.keywordDiamante Formationes_ES
dc.subject.keywordFluvial Systemses_ES
dc.subject.keywordDetrital Modeses_ES
dc.subject.keywordAndean Orogenes_ES
dc.type.versioninfo:eu-repo/semantics/publishedVersiones_ES
dc.origin.lugarDesarrolloUniversidad Nacional de Río Negro. Instituto de Investigación en Paleobiología y Geología.es_ES
dc.relation.journalissue47 (2)es_ES
dc.description.reviewtruees_ES
dc.description.resumenThe Upper Cretaceous nonmarine deposits of the Neuquén Basin have an important regional exposure. These deposits are included in the Neuquén Group, a well-studied unit in both the south and central part of the basin. However, the northernmost exposed between the Laguna del Diamante and the Atuel River - assigned to the Diamante Formation - have not been studied in detail. In the studied area, the Diamante Formation corresponds to a braided fluvial system with moderate sinuosity evolving through time towards an anastomosing fluvial system. Petrographic analyses indicate that sandstones belong to feldspatic litharenites and litharenites, while the source area indicates provenance from both a recycled orogen and a transitional arc. The latter could be linked to the exhumation of the Andean orogen located to the west and to the input from the north-eastern border of the Neuquén Basin, represented by the rocks currently exposed in the San Rafael Block. On a macroscopic scale, the presence of calcareous lithic fragments in the mid and upper part of the surveyed stratigraphic section, strongly suggest an input from the west. This indicates an important change in the polarity of the basin and the presence of a deformation front located to the west of the study area in accordance to previous proposals in equivalent deposits to the south of study area.es_ES
dc.identifier.doihttp://dx.doi.org/10.5027/andgeoV47n2-3218-
dc.relation.journalTitleAndean Geologyes_ES
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