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The geochemistry of the sedimentary rocks from the Huadi No. 1 well in the Wufeng-Longmaxi formations (Upper Ordovician-Lower Silurian), South China, with implications for paleoweathering, provenance, tectonic setting and paleoclimate

EngineeringHuadi NoWufeng-longmaxi FormationsSouth ChinaTectonic EvolutionDetrital ProvenanceGeologyMineral DepositGeochemistryGeochronologyPetrologyEarth ScienceRegional GeologyTectonics