Cretaceous-Tertiary detachment surface, Cerro El Vigía, structural block in the Banámichi-San antonio region, central Sonora, Mexico
Keywords:
Detachment surface, Banámichi-San Antonio region, Sonora, Mexico.
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
Published
2018-11-04
Issue
Section
Regular Papers
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