Browsing by Autor "Michel Fornari"
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Item type: Item , Découverte de vertébrés aquatiques présumés paléocènes dans les Andes septentrionales de Bolivie (Rio Suches, synclinorium de Putina)(Elsevier BV, 1987) Jaime Argollo; Éric Buffetaut; Henri Cappetta; Michel Fornari; Gérard Hérail; Gérard Laubacher; Bernard Sigé; Giovani VizcarraItem type: Item , Late local glacial maximum in the Central Altiplano triggered by cold and locally-wet conditions during the paleolake Tauca episode (17–15ka, Heinrich 1)(Elsevier BV, 2009) Pierre‐Henri Blard; Jérôme Lavé; Kenneth A. Farley; Michel Fornari; Néstor Jiménez; V. RamirezItem type: Item , Late Permian–Middle Jurassic lithospheric thinning in Peru and Bolivia, and its bearing on Andean-age tectonics(Elsevier BV, 2002) Thierry Sempéré; Gabriel Carlier; Pierre Soler; Michel Fornari; Víctor Santiago Carlotto Caillaux; Javier Jacay; Oscar Arispe; Didier Néraudeau; José Cárdenas; Silvia RosasItem type: Item , Progressive glacial retreat in the Southern Altiplano (Uturuncu volcano, 22°S) between 65 and 14 ka constrained by cosmogenic <sup>3</sup>He dating(Cambridge University Press, 2014) Pierre‐Henri Blard; Jérôme Lavé; Kenneth A. Farley; Víctor Ramírez; Néstor Jiménez; Léo Martin; Julien Charreau; Bouchaïb Tibari; Michel FornariAbstract This work presents the first reconstruction of late Pleistocene glacier fluctuations on Uturuncu volcano, in the Southern Tropical Andes. Cosmogenic 3 He dating of glacial landforms provides constraints on ancient glacier position between 65 and 14 ka. Despite important scatter in the exposure ages on the oldest moraines, probably resulting from pre-exposure, these 3 He data constrain the timing of the moraine deposits and subsequent glacier recessions: the Uturuncu glacier may have reached its maximum extent much before the global LGM, maybe as early as 65 ka, with an equilibrium line altitude (ELA) at 5280 m. Then, the glacier remained close to its maximum position, with a main stillstand identified around 40 ka, and another one between 35 and 17 ka, followed by a limited recession at 17 ka. Then, another glacial stillstand is identified upstream during the late glacial period, probably between 16 and 14 ka, with an ELA standing at 5350 m. This stillstand is synchronous with the paleolake Tauca highstand. This result indicates that this regionally wet and cold episode, during the Heinrich 1 event, also impacted the Southern Altiplano. The ELA rose above 5450 m after 14 ka, synchronously with the Bolling–Allerod.Item type: Item , The Central Atlantic Magmatic Province extends into Bolivia(Elsevier BV, 2013) Hervé Bertrand; Michel Fornari; Andrea Marzoli; Raúl García-Duarte; Thierry Sempéré