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- W4224998225 abstract "The Re-Os (rhenium-osmium) chronometer applied to molybdenite (MoS2) is now demonstrated to be remarkably robust, surviving intense deformation and high-grade thermal metamorphism. Successful dating of molybdenite is dependent on proper preparation of the mineral separate and analysis of a critical quantity of molybdenite such that recognized decoupling of 187Re parent and 187Os daughter within molybdenite is overcome. The use of a reference or control sample is necessary to establish laboratory credibility and for inter-laboratory comparisons. High precision, accurate, and reproducible age results are derived through isotope dilution and negative thermal ion mass spectrometry (ID-NTIMS). The laser ICP-MS technique should not be used for Re-Os dating of molybdenite. Successful dating of molybdenite by Re-Os is recognized when Re-Os age results are in agreement with the generally robust U-Pb dating method and with observed geologic relationships. The Rb-Sr, K-Ar, and 40Ar/39Ar chronometers are susceptible to chemical and thermal disturbance, particularly in terranes that have experienced subsequent episodes of hydrothermal/magmatic activity, and therefore should not be used as a basis for establishing accuracy of the Re-Os dating, as has been done in the past." @default.
- W4224998225 created "2022-04-29" @default.
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- W4224998225 date "2022-04-28" @default.
- W4224998225 modified "2023-09-25" @default.
- W4224998225 title "The remarkable Re-Os chronometer in molybdenite: how and why it works (with a comparative look at the Lobash Mo Deposit, Russia)" @default.
- W4224998225 doi "https://doi.org/10.1201/9781003077503-282" @default.
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