Changes

=== Progradating upper section ===

=== Progradating upper section ===

Thickness variability in peliticfacies is marked and corresponds to the distal progradating depositional sequences comprising the high sea cycle portions.<ref>Mitchum, R. M., & M. A. Uliana, 1985, [http://archives.datapages.com/data/specpubs/seismic1/data/a167/a167/0001/0250/0255.htm Seismic stratigraphy of carbonate depositional sequences, Upper Jurassic-Lower Cretaceous, Neuquén Basin, Argentina], in O. R. Berg & D. G. Woolverton (eds.), Seismic Stratigraphy II: An integrated approach to hydrocarbon exploration: [http://store.aapg.org/detail.aspx?id=128 AAPG Memoir 39], p. 255-274.</ref><ref>Carozzi, A. V., I. A. Orchuela, and M. L. Rodriguez Schelotto, 1993, Depositional models of the Lower Cretaceous Quintuco–Loma Montosa Formation, Neuquén Basin, Argentina: Journal of Petroleum Geology, v. 16, 421–450.</ref>

Thickness variability in peliticfacies is marked and corresponds to the distal progradating depositional sequences comprising the high sea cycle portions.<ref>Mitchum, R. M., & M. A. Uliana, 1985, [http://archives.datapages.com/data/specpubs/seismic1/data/a167/a167/0001/0250/0255.htm Seismic stratigraphy of carbonate depositional sequences, Upper Jurassic-Lower Cretaceous, Neuquén Basin, Argentina], in O. R. Berg & D. G. Woolverton (eds.), Seismic Stratigraphy II: An integrated approach to hydrocarbon exploration: [http://store.aapg.org/detail.aspx?id=128 AAPG Memoir 39], p. 255-274.</ref><ref>Carozzi, A. V., I. A. Orchuela, and M. L. Rodriguez Schelotto, 1993, Depositional models of the Lower Cretaceous Quintuco–Loma Montosa Formation, Neuquén Basin, Argentina: Journal of Petroleum Geology, v. 16, 421–450.</ref><ref>Charrier, R., 1985, Estratigrafía, evolución tectónica y significado de las discordancias de los Andes chilenos entre 32°S y 36°S durante el Mesozoico y Cenozoico, ''in'' J. Frutos, R. Oyarzún, and M. Pincheira, eds., Geología y Recursos Minerales de Chile: Concepción, Universidad de Concepción, pp. 101–133.</ref>

Charrier, R., 1985. Estratigrafía, evolución tectónica</ref> Carozzi et al. 1993).

As shown in [[:File:4.png|Figure 4]] facial change area of Vaca Muerta shale in the prograde complex is located inmediately to the west. From east to west the high sea sequence comprises proximal or platformfacies in the entire registry. In the location of CVS.x-1 (see [[:File:4.png|Figure 4]]) a spur is accompanied by a break in paleoestructuralslope where the structural nose would be limited by faults with subtle shift.

As shown in [[:File:4.png|Figure 4]] facial change area of Vaca Muerta shale in the prograde complex is located inmediately to the west. From east to west the high sea sequence comprises proximal or platformfacies in the entire registry. In the location of CVS.x-1 (see [[:File:4.png|Figure 4]]) a spur is accompanied by a break in paleoestructuralslope where the structural nose would be limited by faults with subtle shift.