There is no geological evidence for the participation of fluids mobilized from host rocks in the formation of the CLM.Because the Re-Os chronometer in molybdenite is demonstrably stable through later Variscan facies metamorphism, the molybdenite chronometer has not been affected by subsequent thermal overprints associated with the Variscan orogeny. cookies, tags, and tracking settings to store information that help give you the very best browsing experience.
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We have used this technique to analyze repeatedly a homogeneous molybdenite powder used as a reference standard in our laboratory.