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Role of alternating redox conditions in the formation of organic-rich interval in the Middle Devonian Marcellus Shale, Appalachian Basin, USA

Organic GeochemistryBiogeochemistryFacies AnalysisEngineeringRedox ConditionsOrganic PetrologyAppalachian BasinSedimentary GeologyOrganic-rich Sedimentary RockGeologyGeochemistryPetrologyOrganic-rich IntervalSedimentologyEarth ScienceShale Geology