Changes

Sedimentary basin infill overlying a Devonian to Lower Triassic Gondwanan basement is summarized in five main stages: (1) Late Triassic to Early Jurassic synrift, (2) Early and Middle Jurassic subsidence, (3) Late Jurassic inversion, (4) Late Jurassic–Early Cretaceous subsidence, and (5) Late Cretaceous foreland ([[:file:GiacomoneEtAlFigure3.jpg|Figure 3]]).<ref name=Veigaetal_2020 /><ref name=Llambiasetal_2018>Llambías, E. J., M. Schiuma, D. Velo, M. Barrionuevo, D. Lenge, F. Pángaro, R. Corbera, O. Carbone, and G. Hinterwimmer, 2018, Reservorios del Grupo Choiyoi y Precuyano, in M. Schiuma, G. Hinterwimmer, and G. D. Vergani, eds., Rocas reservorio de las cuencas productivas de Argentina, 2nd ed. [in Spanish]: X Congreso de Exploración y Desarrollo de Hidrocarburos, Mendoza, Argentina, November 5–9, 2018, p. 325–371.</ref><ref name=Ramosetal_2020>Ramos, V. A., M. Naipauer, H. A. Leanza, and M. E. Sigismondi, 2020, An exceptional tectonic setting along the Andean continental margin, in D. Minisini, M. Fantín, I. Lanusse Noguera, and H. A. Leanza, eds., Integrated geology of unconventionals: The case of the Vaca Muerta play, Argentina: AAPG Memoir 121, p. 25–38, doi:10.1306/13682222M1202855.</ref>

Sedimentary basin infill overlying a Devonian to Lower Triassic Gondwanan basement is summarized in five main stages: (1) Late Triassic to Early Jurassic synrift, (2) Early and Middle Jurassic subsidence, (3) Late Jurassic inversion, (4) Late Jurassic–Early Cretaceous subsidence, and (5) Late Cretaceous foreland ([[:file:GiacomoneEtAlFigure3.jpg|Figure 3]]).<ref name=Veigaetal_2020 /><ref name=Llambiasetal_2018>Llambías, E. J., M. Schiuma, D. Velo, M. Barrionuevo, D. Lenge, F. Pángaro, R. Corbera, O. Carbone, and G. Hinterwimmer, 2018, Reservorios del Grupo Choiyoi y Precuyano, in M. Schiuma, G. Hinterwimmer, and G. D. Vergani, eds., Rocas reservorio de las cuencas productivas de Argentina, 2nd ed. [in Spanish]: X Congreso de Exploración y Desarrollo de Hidrocarburos, Mendoza, Argentina, November 5–9, 2018, p. 325–371.</ref><ref name=Ramosetal_2020>Ramos, V. A., M. Naipauer, H. A. Leanza, and M. E. Sigismondi, 2020, An exceptional tectonic setting along the Andean continental margin, in D. Minisini, M. Fantín, I. Lanusse Noguera, and H. A. Leanza, eds., Integrated geology of unconventionals: The case of the Vaca Muerta play, Argentina: AAPG Memoir 121, p. 25–38, doi:10.1306/13682222M1202855.</ref>

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file:GiacomoneEtAlFigure2.jpg|{{figure number|2}}Geological regions of the Neuquén Basin.<ref name=Veigaetal_2020>Veiga, R.D., Vergani, G.D., Brisson, I.E, Macellari, C.E., Leanza, H.A., 2020, The Neuquén Super Basin: AAPG Bulletin, v.104, p. 2521-2555.</ref>

file:GiacomoneEtAlFigure2.jpg|{{figure number|2}}Geological regions of the Neuquén Basin.<ref name=Veigaetal_2020>Veiga, R.D., Vergani, G.D., Brisson, I.E, Macellari, C.E., Leanza, H.A., 2020, The Neuquén Super Basin: AAPG Bulletin, v.104, p. 2521-2555.</ref>

file:GiacomoneEtAlFigure3.jpg|{{figure number|3}}Chronostratigraphic chart of the Neuquén Basin with main reservoirs and source rocks. Tectonic history: cycle climax (solid arrow) versus cycle waning (dotted arrows).<ref name=Veigaetal_2020 />

file:GiacomoneEtAlFigure3.jpg|{{figure number|3}}Chronostratigraphic chart of the Neuquén Basin with main reservoirs and source rocks. Tectonic history: cycle climax (solid arrow) versus cycle waning (dotted arrows).<ref name=Veigaetal_2020 />