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Dissolution of Natural Octahedral Diamonds in an Fe–S Melt at High Pressure

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Abstract—An experimental study was carried out on the dissolution of natural octahedral diamonds from the Internatsionalnaya and Yubileinaya kimberlite pipes (Yakutia) in an Fe–S melt at 4 GPa and 1450–1500°C with different sulfur contents (10–25 wt %). It was found that with an increase in sulfur content in the iron melt, the degree of diamond dissolution sharply decreases. The stationary (final) shape of diamond crystal dissolution under the achieved conditions corresponds to an octahedroid with trigonal etching layers, which is confirmed by photogoniometry. Diamonds with similar morphology are common in kimberlite pipes, especially in mantle xenoliths from kimberlites. It was concluded that diamonds with this shape did not undergo natural dissolution in a kimberlite magma, but, similar to flat-faced octahedra, were probably isolated from it in xenoliths. Therefore, the higher the content of octahedroid-shaped diamonds with trigonal layers in a deposit, the smaller the direct influence of an aggressive kimberlite magma on the diamond content.

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ACKNOWLEDGMENTS

The authors are grateful to the anonymous reviewers for reading the manuscript and valuable comments.

Funding

The study was carried out under the state assignment for the IGM SB RAS with financial support from PJSC ALROSA.

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Authors and Affiliations

  1. Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, 3630090, Novosibirsk, Russia

    V. M. Sonin, E. I. Zhimulev, A. A. Chepurov, E. S. Lindenblot, A. M. Logvinova, V. P. Afanas’ev & A. I. Chepurov

  2. Rzhanov Institute of Semiconductor Physics, Siberian Branch, Russian Academy of Sciences, 3630090, Novosibirsk, Russia

    D. V. Shcheglov

  3. Research and Development Geological Prospecting Enterprise (RDGPE) PJSC ALROSA, 7678170, Mirny, Russia

    B. S. Pomazanskii

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Sonin, V.M., Zhimulev, E.I., Chepurov, A.A. et al. Dissolution of Natural Octahedral Diamonds in an Fe–S Melt at High Pressure. Geol. Ore Deposits 62, 497–507 (2020). https://doi.org/10.1134/S1075701520060070

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