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The Neuquén Basin: Sequence Stratigraphy of Vaca Muerta Formation (view source)
Revision as of 13:37, 16 July 2015
, 13:37, 16 July 2015no edit summary
=== 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 (Mitchum and Uliana, 1985;Carozzi et al. 1993).
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> Carozzi et al. 1993).
As shown in Figure X 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 Figure x) a spur is accompanied by a break in paleoestructuralslope where the structural nose would be limited by faults with subtle shift.
As shown in Figure X 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 Figure x) a spur is accompanied by a break in paleoestructuralslope where the structural nose would be limited by faults with subtle shift.
* Mitchum, R. M. y M. A. Uliana, 1985,. Seismic stratigraphy of carbonate depositional sequences, Upper Jurassic-Lower Cretaceous, Neuquén Basin, Argentina, en Berg O.R. y D. G. Woolverton (eds.), Seismic Stratigraphy II: an integrated approach to hydrocarbon exploration. American Association of Petroleum Geologist, Memoir 39, p. 255-274.
*
* Ramos, V.A. 1999b. Evolución Tectónica de la Argentina. In: CAMINOS, R. (ed.) Geología Argentina. Instituto de Geología y Recursos Minerales, Anales, 29, 715-759.
* Ramos, V.A. 1999b. Evolución Tectónica de la Argentina. In: CAMINOS, R. (ed.) Geología Argentina. Instituto de Geología y Recursos Minerales, Anales, 29, 715-759.
* Tomassini F, Kietzman D, Fatín M, Crousse L, Reijenstein H. Estratigrafía y Análisis de facies de La Formación Vaca Muerta en el área El Trapial, Cuenca Neuquina, Argentina. Simposio de Recursos No Convencionales: ampliando el horizonte energético, 2014. 591-599.
* Tomassini F, Kietzman D, Fatín M, Crousse L, Reijenstein H. Estratigrafía y Análisis de facies de La Formación Vaca Muerta en el área El Trapial, Cuenca Neuquina, Argentina. Simposio de Recursos No Convencionales: ampliando el horizonte energético, 2014. 591-599.