Cordón de Lila-Sierra de Almeyda Cambro-Ordovicic batholith: geochemistry of the plutonic rocks. Antofagasta region ,Chile
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DOI: 10.5027/andgeov47n3-3305
Abstract: An Upper Cambrian-Ordovician (490-460 Ma) batholith crop out along the Cordon de Lila and Sierra de Almeida, in the Antofagasta region, northern Chile, which belongs to the Famatinian arc. Two plutonic rock types can be… read more here.
Keywords: antofagasta region; batholith; lila sierra; geochemistry ... See more keywords