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Early Paleozoic mantle diapirism in Galicia
Authors:E.J Keasberry   P.W.C Van Calsteren  R.P Kuijper
Abstract:Comparison of the geological outcrop and the Bouguer map of the Ordenes Complex in Galicia (NW Spain), gives substantial evidence for a subdivision of the peripheral belt into separate units. These units, high-grade metamorphic complexes, appear to have their origin in diapiric movements of upper-mantle material into a crystalline lower crust of continental type.
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