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[[File:4.png|400px|thumbnail|{{figure number|4}}Cuts estratigráfico leveled to the ceiling of the Group Low Mendoza, where there are observed the interpreted sequences and its facial changes inside the complex progradante.<ref>Borbolla M. C., C. Cruz, J. Villar, N. Annizzotto, P. Benites, D. Cattaneo, 2014, Formación Vaca Muerta: variación lateral de facies y su implicancia en los cambios de espesor hacia el borde de cuenca. Perspectivas exploratorias en shale oil e la plataforma de Catriel,  Cuenca Neuquina,Argentina. Simposio de Recursos No Convencionales: ampliando el horizonte energético, pp. 321-329</ref>]]
 
[[File:4.png|400px|thumbnail|{{figure number|4}}Cuts estratigráfico leveled to the ceiling of the Group Low Mendoza, where there are observed the interpreted sequences and its facial changes inside the complex progradante.<ref>Borbolla M. C., C. Cruz, J. Villar, N. Annizzotto, P. Benites, D. Cattaneo, 2014, Formación Vaca Muerta: variación lateral de facies y su implicancia en los cambios de espesor hacia el borde de cuenca. Perspectivas exploratorias en shale oil e la plataforma de Catriel,  Cuenca Neuquina,Argentina. Simposio de Recursos No Convencionales: ampliando el horizonte energético, pp. 321-329</ref>]]
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The basal transegresive sequence in this sector of the basin retains the characteristics of sourcerock constant across large areas.<ref>Veiga, R. D., & I. A. Orchuela, 1989, Identificación de niveles generadores de hidrocarburos a partir de técnicas de perfilaje en la formación Vaca Muerta. I Congreso Nacional de Exploración de Hidrocarburos, p. 1061-1093. Mar del Plata, Argentina.</ref>
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The basal transgressive sequence in this sector of the basin retains the characteristics of sourcerock constant across large areas.<ref>Veiga, R. D., & I. A. Orchuela, 1989, Identificación de niveles generadores de hidrocarburos a partir de técnicas de perfilaje en la formación Vaca Muerta. I Congreso Nacional de Exploración de Hidrocarburos, p. 1061-1093. Mar del Plata, Argentina.</ref>
    
The Lowstand System Tract (LST) is not present, the Transgressive System Tract (TST) is very small and corresponds to the regional flood event. The section is dominated by high sea deposits prograding (Highstand System Tracts) where three subsequenceares individualized: A, B and C.
 
The Lowstand System Tract (LST) is not present, the Transgressive System Tract (TST) is very small and corresponds to the regional flood event. The section is dominated by high sea deposits prograding (Highstand System Tracts) where three subsequenceares individualized: A, B and C.

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