Abstract
Five sedimentary facies were distinguished in the two outcrops studied and were interpreted in the following manner: one facies represents the deposition at the bottom of the basin (black shale facies); three facies represent a turbiditic lobe (facies of sandy rhytmites, facies of shaly rhytmites, and facies of lenticular sandstones); and the last is a slumping facies representing a slope deposition (green shale facies). After this, the work proceeded with the integration of the data obtained with the litostratigraphy of the Reconcavo Basin.
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