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Titlebook: Geological Records of the Fuegian Andes Deformed Complex Framed in a Patagonian Orogenic Belt Region; Rogelio Daniel Acevedo Book 2019 The

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Nature and Synthesis of the Results Obtained,cks in the Fuegian Andes. This has been done in this way based upon the idea that an integration of the data as well as interpretations and emerging ideas can be, to an acceptable extent, separated from the data themselves.
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A Simplified View About the Fuegian Andes and the Complex Folding of the Mesozoic and Early Tertiarindependent phenomena. The Patagonian Cordillera from Lake Fontana (44º 56’ S, 71º 30’ W) to the south shows a simple architecture in strong contrast with the one of the Fuegian folding already outlined in the southernmost sector of the N-S belt, that is, north of the Fuegian arc.
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Rogelio Daniel AcevedoPerforms an appraisal of the development and valorization of formations of the Jurassic and early Cretaceous to reach the simple scheme of the Fuegian-Patagonian geologic continuity under the name of
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https://doi.org/10.1007/978-3-662-26110-1ibed as vein-layer interbedding in the sedimentary frame of the Yahgan Fm. and were joined later to the Lemaire Fm. as an expression of bimodal volcanism to explain the mineralization model of the volcanogenic massive sulfides.
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https://doi.org/10.1007/978-3-642-92121-6Montes Negros and Atocha, Campana and Pirámide hills are situated there, at the southern coast, and the Arriola, Real, and Bilbao hills at the northern coast. Beyond the Straits of Le Maire, the Isla Grande de Tierra del Fuego is separated from Isla de los Estados, whose geologic continuity with the
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