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The Malaguide basement is formed by a thick, strongly deformed but weakly metamorphosed sedimentary succession of ?Ordovician-Carboniferous age, mainly made of basinal mudstones and turbidites, which includes a thin but conspicuous Lower Carboniferous chert-limestone interval (Falcona formation). The chert member (ribbon radiolarites) yielded, for the first time in Southern Spain, Tournaisian radiolarians...
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