Large S isotope and trace element fractionations in pyrite of uranium roll front systems result from internally-driven biogeochemical cycle
Christophe Bonnetti, Lingli Zhou, Thomas Riegler, Joël Brugger, Martin Fairclough
Topics & Concepts
PyriteTrace elementSulfateGeologyBiogeochemical cycleδ34SSulfurChemistrySulfur cycleMineralogyGeochemistryEnvironmental chemistryHydrothermal circulationFluid inclusionsPaleontologyOrganic chemistryRadioactive element chemistry and processingGeological and Geochemical AnalysisMine drainage and remediation techniques