Titlebook: Gondwana Landscapes in southern South America; Argentina, Uruguay a Jorge Rabassa,Cliff Ollier Book 2014 Springer Science+Business Media Do

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https://doi.org/10.1007/978-3-642-18693-6he surface carved in the oldest rocks is located at intermediate elevations. The Vacaria Surface evolved during the Late Cretaceous and the Paleogene, whereas the Ca?apava do Sul Surface has an even older development, typically corresponding in this area to the Gondwana Surface, with some particular

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https://doi.org/10.1007/978-3-476-03004-7rly Tertiary, when very wet and warm conditions were established, in coincidence with the “Palaeocene–Eocene Thermal Maximum (PETM)”, followed by semiarid climates in the Oligocene, wetter conditions in the Miocene and semiarid again in the Pliocene, with alternating semiarid and humid conditions du

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Frauen, Lust und sexuelles Wohlbefindenbrian gneissic-migmatitic rocks (the Monte Guazú Complex), mylonites and ultramylonites (the Guacha Corral shear zone), and Devonian granites (the Cerro áspero Batholith). The latter are accompanied by fluorite epithermal mineralizations (Early Cretaceous). The paleosurfaces were affected by the And