Geochemistry International

, Volume 45, Issue 6, pp 538–545 | Cite as

Mantle(?) xenoliths in the carbonatites of northern Transbaikalia

  • G. S. Ripp
  • A. G. Doroshkevich
  • M. V. Badmatsyrenov
  • N. S. Karmanov


The composition and nature of high-Cr minerals in lithic clasts from the carbonatites of the Veseloe occurrence, northern Transbaikalia, were considered. In order to determine their source, the Cr-bearing phases were compared with chromite, magnetite, and rutile from ultrabasic rocks, mantle xenoliths, and eclogites. It was suggested that the xenoclasts studied were formed at great depths, whereas the carbonatites were directly derived from the mantle rather than formed by the crustal differentiation of a silicate-carbonate melt.


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Copyright information

© Pleiades Publishing, Ltd. 2007

Authors and Affiliations

  • G. S. Ripp
    • 1
  • A. G. Doroshkevich
    • 1
  • M. V. Badmatsyrenov
    • 1
  • N. S. Karmanov
    • 1
  1. 1.Geological Institute, Siberian DivisionRussian Academy of SciencesUlan-UdeRussia

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