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Mario Vergara,Beatriz Levi,Jan O. Nystrom,Eugenia Fonseca,Carlos Roeschmann
Pág. 295 - 302
ABSTRACT. Stratigraphic sequences of Lower Cretaceous age occur in two belts along central Chile. Between 30° and 35°S, the western belt, situated in the Coast Range is composed of 7-14 km thick intra-arc and forearc sequences dominated by shoshonitic to...
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