Related Experiment Video
Updated: Jul 11, 2026

09:41
Isolation of Quartz Grains for Optically Stimulated Luminescence (OSL) Dating of Quaternary Sediments for Paleoenvironmental Research
Published on: August 2, 2021
Quartz and magnetite: oxygen-18-oxygen-16 fractionation in metamorphosed biwabik iron formation
Abstract:
Oxygen-18-oxygen-16 fractionation of coexisting quartz and magnetite from the Biwabik iron formation varies as a function of distance of the sample from an intrusive contact. This isotope fractionation is related to observed mineralogic variations and compared with a theoretical heat-flow model.
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