01945nmc a2200205 4500 20260520010331.0 260224s xxu CD I116 64 0015469 Geología del ciclo neocomiano superior, caracterización litológica y discriminación de subambientes deltaicos en la zona de río Mayo, sector noroccidental de la Cuenca del Golfo San Jorge 10/11/2016 ; 10/11/2016 23 p. Geology, lithology and deltaic sub-environments discrimination in the Upper Neocomian of the Río Mayo area, Northwestern sector of the San Jorge Basin The aim of this study is to analyze the geology of the Neocomian cycle focused in the upper section of Pozo Cerro Guadal Formation. The lithological characterization of this unit has been performed by core and cutting descriptions and the interpretation of well logs in order to recognize the existing lithofacies and the associated prograding successions. Considering a deltaic facies model it has been possible to associate the recognized lithofacies to their corresponding depositional environments. Paleogeographic maps have been generated from the facies successions ́analysis and the correlation of the defined prograding sequences. Within a tectonostratigraphic context, the paleogeographic and paleoenvironmental reconstruction are useful to explain the relative reservoir and non reservoir facies distribution in each deltaic environment. The understanding of this conceptual model intends to be a guide in the construction of a geocelular model. . CONGTP Catalano, Juan Pablo 51300 Ramos, Juan José 55742 Congreso de Exploración y Desarrollo de Hidrocarburos (9no. : 2014 nov. 3-7 : Mendoza) 54287 189822 189822 https://biblioteca.iapg.org.ar/ArchivosAdjuntos/CONEXPLOR2014/431-Geologiadelciclo.pdf 0 0 0 0 257641 BAAB BAAB CD I116 64 0015469 2026-03-06 200062068 0 CD I116 64 0015469 200062068 2026-03-06 00:19:58 2026-03-06 ARCHIVO