Publication | Open Access

Framboidal pyrite evidence for persistent low oxygen levels in shallow-marine facies of the Nanpanjiang Basin during the Permian-Triassic transition

Permian-triassic TransitionOrganic GeochemistryMarine GeologyEngineeringNanpanjiang BasinGeologyOxygen IsotopeGeochemistrySedimentary PetrologyGeochronologyPetrologyFramboidal Pyrite EvidenceEarth Science