Inclusions of Cr- and Cr–Nb-Rutile in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia
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The results of study of rutile inclusions in pyrope from the Internatsionalnaya kimberlite pipe are presented. Rutile is characterized by unusually high contents of impurities (up to 25 wt %). The presence of Cr2O3 (up to 9.75 wt %) and Nb2O5 (up to 15.57 wt %) are most typical. Rutile inclusions often occur in assemblage with Ti-rich oxides: picroilmenite and crichtonite group minerals. The Cr-pyropes with inclusions of rutile, picroilmenite, and crichtonite group minerals were formed in the lithospheric mantle beneath the Mirnyi field during their joint crystallization from melts enriched in Fe, Ti, and other incompatible elements as a result of metasomatic enrichment of the depleted lithospheric mantle.
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- 4.S. E. Haggerty, Rev. Mineral. 25, 355–416 (1991).Google Scholar
- 5.K. D. Litasov, Y. D. Litasov, V. G. Malkovets, and H. Taniguchi, J. Northeast Asian Stud. 10, 161–175 (2006).Google Scholar
- 8.D. A. Varlamov, V. K. Garanin, and S. I. Kostrovitskiy, Dokl. Akad. Nauk 345 3, 364–366 (1995).Google Scholar
- 9.G. L. Davis, N. V. Sobolev, and A. D. Khar’kiv, Dokl. Akad. Nauk 254 1, 175–179 (1980).Google Scholar
- 10.N. V. Sobolev, Geol. Geofiz. 12 3, 70–80 (1971).Google Scholar
- 12.D. G. Pearson, S. B. Shirey, R. W. Carlson, R. R. Boyd, N. P. Pokhilenko, and N. Shimizu, Geochim. Cosmochim. Acta 59, 959–977 (1995).Google Scholar
- 14.V. G. Malkovets, W. L. Griffin, N. J. Pearson, et al., in Proc. 10th Int. Kimberlite Conf. (Bangalore, 2012), Long Abstract 10IKC-173.Google Scholar