Abstract
The Cerro El Vigía, in east-central Sonora, is a structural block that was detached along a major low-angle fault. This fault, La Ramada-Agua Caliente detachment fault, separates an autochthonous early Tertiary igneous complex (the Aconchi batholith) from chaotically deformed Paleozoic and Early Cretaceous strata in Cerro El Vigía… in order to continue, download the full paper in PDF
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