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Composition of the Ordovician lithospheric mantle: Evidence from the study of peridotite xenoliths from camptonite of the Sangilen highland, central Asian fold belt

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Authors and Affiliations

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

    A. A. Gibsher, V. G. Malkovets, K. D. Litasov, Yu. D. Litasov & N. P. Pokhilenko

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  1. A. A. Gibsher
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  2. V. G. Malkovets
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  3. K. D. Litasov
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  4. Yu. D. Litasov
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  5. N. P. Pokhilenko
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Correspondence to A. A. Gibsher.

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Original Russian Text © A.A. Gibsher, V.G. Mal’kovets, K.D. Litasov, Yu.D. Litasov, N.P. Pokhilenko, 2010, published in Doklady Akademii Nauk, 2010, Vol. 433, No. 3, pp. 369–373.

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Gibsher, A.A., Malkovets, V.G., Litasov, K.D. et al. Composition of the Ordovician lithospheric mantle: Evidence from the study of peridotite xenoliths from camptonite of the Sangilen highland, central Asian fold belt. Dokl. Earth Sc. 433, 957–961 (2010). https://doi.org/10.1134/S1028334X1007024X

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  • DOI: https://doi.org/10.1134/S1028334X1007024X

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