Provenance and paleogeography of the Devonian Durazno Group, southern Parana Basin in Uruguay
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The Devonian Durazno Group as part of the Paraná Basin was deposited in an extensional basin.

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Its provenance is determined by petrography, geochemistry and detrital zircon dating.

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U–Pb detrital zircon age populations indicate main sources related to the Neoproterozoic, whereas minor record Mesoproterozoic rocks.

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Provenance from the Cuchilla Dionisio-Dom Feliciano, Nico Pérez and Piedra Alta terranes (Uruguay-Brazil) is evident.

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Source rocks and paleogeographical implications in SW Gondwana are compared and discussed.

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