Abstract
Direct dating of corundum and the establishment of age constraints for corundum crystal growth are restricted due to the absence of a geochronometer. Syngenetic mineral inclusions may help define minimum ages for corundum growth. Here, we present results of in situ LA-ICP-MS U–Pb dating applied to rutile inclusions in corundum from localities along the Mozambique belt. U–Pb dating of rutile inclusions gave ages of 533 ± 11 Ma (2 σ) for the Gitonga pit (John Saul ruby mine) and 526 ± 13 Ma for the Aqua Ruby mine, both in the Mangari area of Kenya, and an age of 499 ± 12 Ma for ruby from the Morogoro area, Tanzania. These ages are interpreted as cooling ages that set a minimum age for corundum growth following metamorphism along the East-African Antarctic Orogen, and might be used for petrogenetic tracing of corundum in placer deposits.
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Acknowledgments
We are thankful to the vice president of Johannes Gutenberg University Mainz (JGU), Prof. Dr. Wolfgang Hofmeister, and the Institute for Geosciences of JGU for providing samples used in this study. The research has been supported by scholarship A-13-00099 of the German Academic Exchange Service (DAAD) and Institute for Geosciences of JGU. We also thank reviewer Dr. Thomas Zack for helpful suggestions and Prof. Dr. Bernd Lehmann for editing the manuscript.
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Sorokina, E.S., Rösel, D., Häger, T. et al. LA-ICP-MS U–Pb dating of rutile inclusions within corundum (ruby and sapphire): new constraints on the formation of corundum deposits along the Mozambique belt. Miner Deposita 52, 641–649 (2017). https://doi.org/10.1007/s00126-017-0732-x
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DOI: https://doi.org/10.1007/s00126-017-0732-x