Cartografia do sinclinal de Buçaco-Penedos de Góis

Abstract

At a normal fieldwork scale (1/25000) problems arise in the cartographic representation of some of the units defined in the Buçaco-Penedo de Góis syncline, which have thicknesses of 50 meters or less. It was necessary to group them resulting in a lithostratigraphic sequence for most of the cartographic separations already carried out by Delgado (1908), although with the designations created by later authors.