V–Cr–Nb–W-Bearing Rutile in Metamorphic Rocks of the Slyudyanka Complex, Southern Baikal Region


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Abstract

The paper presents data on accessory rutile in Cr–V-rich metamorphic rocks of the Slyudyanka crystalline (granulite) complex in the southern Baikal region. The geochemical features of the studied rutile are unique in combining isomorphic admixtures typical of the mineral from either mafic (Cr) or felsic igneous and associated metasomatic rocks (W), as well as the Nb and V contents, which are abnormally high for metamorphic rocks. The highest concentrations of these elements are as follows, wt %: 15.38 V2O3, 4.33 Cr2O3, 11.09 Nb2O5, 12.36 WO3. These high W and V contents have never been measured in natural rutile. The studied rutile is compared to that from other Cr–V-bearing rocks in the world and various genetic types. The optimal isomorphic substitutions and probable conditions of their realization are discussed.

About the authors

L. Z. Reznitsky

Institute of the Earth’s Crust

Author for correspondence.
Email: garry@crust.irk.ru
Russian Federation, ul. Lermontova 128, Irkutsk, 664033

E. V. Sklyarov

Institute of the Earth’s Crust; Far Eastern Federal University

Email: garry@crust.irk.ru
Russian Federation, ul. Lermontova 128, Irkutsk, 664033; ul. Sukhanova 8, Vladivostok, 690950

L. F. Suvorova

Institute of Geochemistry

Email: garry@crust.irk.ru
Russian Federation, ul. Favorskogo 1A, Irkutsk, 664033

I. G. Barash

Institute of the Earth’s Crust

Email: garry@crust.irk.ru
Russian Federation, ul. Lermontova 128, Irkutsk, 664033

N. S. Karmanov

Institute of Geology and Mineralogy Siberian Branch Russian Academy of Sciences

Email: garry@crust.irk.ru
Russian Federation, pr. Koptyuga 3, Novosibirsk, 630090

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