2019
DOI: 10.1016/j.gsf.2017.12.019
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The Puesto Piris Formation: Evidence of basin-development in the North Patagonian Massif during crustal extension associated with Gondwana breakup

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Cited by 21 publications
(6 citation statements)
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“…The Marifil Volcanic Complex (Figure 1) represents the Lower Jurassic. Its lower section, the Puesto Piris Formation (Núñez et al., 1975), includes conglomerate, sandstone, limestone and tuff of continental rift origin (Strazzere et al., 2019). The upper section is compounded by a thick sequence of ignimbrites, tuff, volcanic breccias and subvolcanic bodies assigned to the Aguada del Bagual and La Porfia formations.…”
Section: Geological Settingmentioning
confidence: 99%
“…The Marifil Volcanic Complex (Figure 1) represents the Lower Jurassic. Its lower section, the Puesto Piris Formation (Núñez et al., 1975), includes conglomerate, sandstone, limestone and tuff of continental rift origin (Strazzere et al., 2019). The upper section is compounded by a thick sequence of ignimbrites, tuff, volcanic breccias and subvolcanic bodies assigned to the Aguada del Bagual and La Porfia formations.…”
Section: Geological Settingmentioning
confidence: 99%
“…1999;Rapela et al . 2000;Strazzere et al . 2017;Pavón Pivetta et al 2019Gordon and Ort, 1994, Rapela et al .…”
Section: -The Early Jurassic Volcanism Of Central Patagonia Forms An Extensiveunclassified
“…Although the radiometric ages of these rocks start in the Middle Triassic and continue until the Middle Jurassic, González et al (2017a) pointed out that there are two main groups of ages for this range between Valcheta and Sierra Grande towns: Middle Triassic (Cortés, 1981;Genovese, 1995;González et al, 2014González et al, , 2017b; and Early Jurassic (Rapela and Pankhurst, 1993;Pankhurst and Rapela, 1995;Strazzere et al, 2019). Younger ages (Middle Jurassic) were obtained southwards in Península Camarones and Dique Ameghino (Feraud et al, 1999;Pankhurst et al, 2000).…”
Section: Marifil Volcanic Complexmentioning
confidence: 99%
“…This unit was defined by Nuñez et al (1975) for epiclastic rocks at the base of Mesozoic volcanicsedimentary sequences laying on Palaeozoic units. This formation is a 150 m to 550 metresthick sequence that has a grain-decreasing tendency and includes thick beds of conglomerate at the base grading to sandstones, limestones and siltstones at the top of the sequence (Nuñez et al, 1975;Strazzere et al, 2019). These rocks have been related to the evolution of highenergy fluvial currents to low-energy fluvial and lacustrine (Strazzere et al, 2019).…”
Section: Marifil Volcanic Complexmentioning
confidence: 99%
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