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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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楼主: 戏弄
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Background,The study of the geologic features of the Argentinian Fuegian Andes has been rich in results and publications both from local and foreign scientists.
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Western Sector of the Fuegian Andes Deformed Complex (FADC-WS),The Mesozoic complex starts here from the simplest chronostratigraphic chart, consisting of a thick marine layer of Late Jurassic–Early Cretaceous age, superimposed to Jurassic volcanic and sedimentary rocks and overlain by Late Cretaceous marine sedimentary rocks, the whole sequence folded and metamorphosed.
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The Estimated Basement of the Fuegian Andes Mesozoic Stratigraphic Series and Those Rocks Regarded It was already pointed out the possible role of the “.” as basement, as a consequence of the regional extension of the quartz porphyries in Patagonia. This would be a restricted concept of the word basement, as stated before.
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The Synthesis About the Formational Matter-Lithostratigraphic Units,The high nomenclatural complexity of the present analysis is shown by the fact that, before the Early Cretaceous, the geological literature records a lot of formational names, fruit of the contributions of many different authors.
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Eastern Sector of the Fuegian Andes Deformed Complex (FADC-ES),Montes 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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