The Vaca Muerta-Quintuco system (Tithonian-Valanginian) in the Neuquén Basin, Argentina: A view from the outcrops in the Chos Malal fold and thrust belt

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The Vaca Muerta-Quintuco system (uppermost lower Tithonian-lower Valanginian) is a thick shallowing-upward sedimentary cycle consisting of dark bituminous shales, marlstones, limestones, and sandstones, cropping out in the Neuquén Basin, west-central Argentina. This paper analyzes three outcrop sect...

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Autor principal: Kietzmann, D.A
Otros Autores: Ambrosio, A.L, Suriano, J., Alonso, M.S, Tomassini, F.G, Depine, G., Repol, D.
Formato: Capítulo de libro
Lenguaje:Inglés
Publicado: American Association of Petroleum Geologists 2016
Materias:
CARBON
ARGENTINA
NEUQUEN BASIN
Acceso en línea:Registro en Scopus
DOI
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Registro en la Biblioteca Digital
Aporte de:Registro referencial: Solicitar el recurso aquí
Biblioteca Central Dr. Luis F. Leloir (FCEN) de Universidad de Buenos Aires
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100 1 |a Kietzmann, D.A. 
245 1 4 |a The Vaca Muerta-Quintuco system (Tithonian-Valanginian) in the Neuquén Basin, Argentina: A view from the outcrops in the Chos Malal fold and thrust belt 
260 |b American Association of Petroleum Geologists  |c 2016 
506 |2 openaire  |e Política editorial 
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504 |a Wright, L.D., Friedrichs, C.T., Kim, S.C., Scully, M.E., Effects of ambient currents and waves on gravity-driven sediment transport on continental shelves (2001) Marine Geology, 175, pp. 25-45 
504 |a Zeiss, A., Leanza, H.A., Interesting new ammonites from the Upper Jurassic of Argentina and their correlation potential: New possibilities for global correlations at the base of the Upper Tithonian by ammonites, calpionellids and other fossil groups (2008) Newsletters on Stratigraphy, 42, pp. 223-247 
520 3 |a The Vaca Muerta-Quintuco system (uppermost lower Tithonian-lower Valanginian) is a thick shallowing-upward sedimentary cycle consisting of dark bituminous shales, marlstones, limestones, and sandstones, cropping out in the Neuquén Basin, west-central Argentina. This paper analyzes three outcrop sections in Chos Malal area, northem Neuquén province. Detailed facies analysis allows us to differentiate six facies associations, representing basinal to proximal outer ramp facies of a homoclinal carbonate ramp system (Vaca Muerta Formation) and basinal to shoreface facies of a mixed carbonate-siliciclastic shelf system (Quintuco Formation), prograding westward from the eastern margin of the basin. Two sequence hierarchies were recognized: 5 composite depositional sequences (third order) and 15 high-frequency sequences (fourth order). Fluctuations in organic matter content within the Vaca Muerta Formation suggest a relationship with depositional sequences, finding the highest values associated with transgressive systems tract, whereas the transition to the Quintuco Formation shows a strong decrease in total organic carbon. The xray diffraction studies showan increase of clayminerals and quartz in the transgressive systems tract of the Vaca Muerta Formation and an increase in the content of calcite in highstand systems tracts. This pattern is reversed in the Quintuco Formation. Our sequence stratigraphic approach contributes to the understanding of the relationship between organic matter, clay minerals, facies, stacking pattern, and relative sea level changes in this exceptional shale oil and shale gas unconventional reservoir. This study may be helpful for a better postulate of petrophysical and geomechanical models for unconventional exploration. Copyright © 2016. The American Association of Petroleum Geologists. All rights reserved.  |l eng 
593 |a Instituto de Estudios Andinos Don Pablo Groeber, Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Consejo Nacional de Investigaciones Científicas y Técnicas, Ciudad Universitaria, Pabellón II, Intendente Güiraldes 2160, Ciudad Autónoma de Buenos Aires, C1428EHA, Argentina 
593 |a Geoandina SRL, Ciudad de la Paz 3257, Piso 6 D, Ciudad Autónoma de Buenos Aires, C1429ACG, Argentina 
593 |a Instituto de Geociencias Básicas, Ambientales y Aplicadas, Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Consejo Nacional de Investigaciones Científicas y Técnicas, Ciudad Universitaria, Pabellón II, Intendente Güiraldes 2160, Ciudad Autónoma de Buenos Aires, C1428EHA, Argentina 
593 |a Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Ciudad Universitaria, Pabellón II, Intendente Güiraldes 2160, Ciudad Autónoma de Buenos Aires, C1428EHA, Argentina 
593 |a Shell Exploration and Production Company, 200 N Dairy Ashford Rd, Houston, TX 77079, United States 
690 1 0 |a BIOGEOCHEMISTRY 
690 1 0 |a BIOLOGICAL MATERIALS 
690 1 0 |a COASTAL ZONES 
690 1 0 |a DEPOSITION 
690 1 0 |a ORGANIC COMPOUNDS 
690 1 0 |a ORGANIC MINERALS 
690 1 0 |a PETROLEUM GEOLOGY 
690 1 0 |a SEA LEVEL 
690 1 0 |a SHALE 
690 1 0 |a SHALE OIL 
690 1 0 |a STRATIGRAPHY 
690 1 0 |a TECTONICS 
690 1 0 |a CARBONATE RAMP SYSTEM 
690 1 0 |a DEPOSITIONAL SEQUENCES 
690 1 0 |a HIGHSTAND SYSTEMS TRACT 
690 1 0 |a ORGANIC MATTER CONTENT 
690 1 0 |a RELATIVE SEA-LEVEL CHANGES 
690 1 0 |a TRANSGRESSIVE SYSTEMS TRACTS 
690 1 0 |a UNCONVENTIONAL RESERVOIRS 
690 1 0 |a X-RAY DIFFRACTION STUDIES 
690 1 0 |a ORGANIC CARBON 
690 1 0 |a BITUMEN 
690 1 0 |a CARBONATE RAMP 
690 1 0 |a CLAY MINERAL 
690 1 0 |a CYCLIC SEDIMENTATION 
690 1 0 |a DEPOSITIONAL SEQUENCE 
690 1 0 |a FACIES ANALYSIS 
690 1 0 |a FOLDING 
690 1 0 |a OIL SHALE 
690 1 0 |a ORGANIC MATTER 
690 1 0 |a SEA LEVEL CHANGE 
690 1 0 |a THRUST FAULT 
650 1 7 |2 spines  |a CARBON 
651 4 |a ARGENTINA 
651 4 |a NEUQUEN BASIN 
700 1 |a Ambrosio, A.L. 
700 1 |a Suriano, J. 
700 1 |a Alonso, M.S. 
700 1 |a Tomassini, F.G. 
700 1 |a Depine, G. 
700 1 |a Repol, D. 
773 0 |d American Association of Petroleum Geologists, 2016  |g v. 100  |h pp. 743-771  |k n. 5  |p AAPG Bull.  |x 01491423  |w (AR-BaUEN)CENRE-786  |t AAPG Bulletin 
856 4 1 |u https://www.scopus.com/inward/record.uri?eid=2-s2.0-85015442323&doi=10.1306%2f02101615121&partnerID=40&md5=6b04f40ddec1d40e426556b678b10d81  |y Registro en Scopus 
856 4 0 |u https://doi.org/10.1306/02101615121  |y DOI 
856 4 0 |u https://hdl.handle.net/20.500.12110/paper_01491423_v100_n5_p743_Kietzmann  |y Handle 
856 4 0 |u https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_01491423_v100_n5_p743_Kietzmann  |y Registro en la Biblioteca Digital 
961 |a paper_01491423_v100_n5_p743_Kietzmann  |b paper  |c PE 
962 |a info:eu-repo/semantics/article  |a info:ar-repo/semantics/artículo  |b info:eu-repo/semantics/publishedVersion 
999 |c 76966 

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