000			03099nmc a2200277 4500
005			20260520010355.0
008			260224s2018 xxu esp
041			_aEspañol
082			_a068.82 553.28 C62 2018 0015655
245	0	0	_aEsquema estratigráfico secuencial a partir de la integración de cuttings, perfiles y sísmica. Formación Quintuco y Vaca Muerta, Cuenca Neuquina
260			_a _b _c2018
270			_a01/07/2022 ; 01/03/2019
300			_a14 p. ; 113-137
520			_aThe Vaca-Muerta- Quintuco (VM-Q) (Middle Tithonian-Lower Valanginian) mixed system is one of the most prolific unconventional shale oil and gas plays outside the USA. Deposition was dominated by marine deposits where VacaMuerta Formation (VMFm.) represents the basinal, northwest-ward prograding shale/carbonate units and Quintuco Formation (QFm.) corresponds to shallow marine, more aggrading carbonate-dominated mixed deposits. Lithostratigraphic boundaries are diachronous where VMFm. is the time equivalent basinal succession to the shelfal, higher energy QFm.A high-resolution sequence stratigraphic framework was established to contribute to the understanding of the VM-Q second order transgressive-regressive mixed clastic-carbonate sequence. Based on the integration of a large multi survey 3D/2D seismic database with well data and geochemistry information, a regional 3D geological conceptual model was built that captures the heterogeneities at different scales. The model incorporates more than 2900 petrographic data points from cuttings over 23 wells distributed along the basin. Textural components, mineralogy, organic matter content and fossil distribution were analyzed and cross-correlated with wireline logs and seismic data. This study documents the 3D polarity and variability of the system on both dip and strike directions based on the interpretation of several regional cross-sections. Main interpreted seismic horizons were calibrated with higher-frequency cycles interpreted from well cuttings. Within the eight seismic sequences, facies associations vary according to their position within the depositional profile: a) shelf interior deposits represented mainly by carbonate-rich facies in the southeast coeval with more mixed facies towards the southwest; b) Slope deposits characterized by monotonous wacke-packestone facies, and c) basinal deposits showing the highest TOC content in the oldest transgressive sequence, progressively decreasing in younger and more proximal basinal facies.
773			_g
942			_cCONGTP
100	1		_aGodino, Georgina _951897
100	1		_aGiunta, David _958446
111	2		_aCongreso de Exploración y Desarrollo de Hidrocarburos (10mo. : 2018 nov. 5 - 9 : Mendoza) _9573
111	2		_aSimposio de Recursos No Convencionales (2018 nov. 5 - 9 : Mendoza) _9781
650		0	_aFormación Vaca Muerta _9679
650		0	_aFacies _958447
650		0	_aModelado geológico _958448
999			_c192689 _d192689
856			_uhttps://biblioteca.iapg.org.ar/ArchivosAdjuntos/Conexplor2018/SRNC/1114.pdf