In this paper a new tectono-stratigraphic subdivision far the materials from the Badajoz-Córdoba Shear Belt based on field geology and P-T metamorphic analitical data is suggested. Five stacked slices with different lithological features and metamorphic histories constitute an allochthonous tectonic pile of Upper Precambrian age. The stack overrides a lower-grade pelitic para-authochthonous during the regional D, Pan-African-Cadomian orogenic event.
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