The zircon evidence of temporally changing sediment transport—the NW Gondwana margin during Cambrian to Devonian time (Aoucert and Smara areas, Moroccan Sahara)
The zircon evidence of temporally changing sediment transport—the NW Gondwana margin during Cambrian to Devonian time (Aoucert and Smara areas, Moroccan Sahara)
Authors
Keywords
U–Th–Pb geochronology, Zircon morphology, Zircon from limestone, West African Craton, Palaeozoic sediment transport
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