gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2017-8-3-0277gtcrust-418Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSANALYSIS OF THE CHEMICAL COMPOSITION OF CHAROITE ROCKSANALYSIS OF THE CHEMICAL COMPOSITION OF CHAROITE ROCKSMarchukM. V.MarchukM. V.

Irkutsk

Irkutsk

SokolovaT. S.SokolovaT. S.

Irkutsk

Irkutsk

LevinA. V.LevinA. V.

Irkutsk

Irkutsk

Institute of the Earth’s crust, Siberian Branch of RASРоссияInstitute of the Earth’s crust, Siberian Branch of RASRussian Federation20171210201783511513Copyright © Marchuk M.V., Sokolova T.S., Levin A.V., 20172017Marchuk M.V., Sokolova T.S., Levin A.V.Marchuk M.V., Sokolova T.S., Levin A.V.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/418

The unique charoite mineralization, established on the Murun alkaline massif in the northwestern part of the Aldan shield on the border of the Irkutsk region and Yakutia, is still of great interest to some of researchers (geologists, crystallographers, geochemists, etc.). The outcrops of charoite-bearing rocks at the “Sirenevyi Kamen” deposit are noted both in the indigenous outcrops and in eluvial clatters [Bondarenko, 2009].

The unique charoite mineralization, established on the Murun alkaline massif in the northwestern part of the Aldan shield on the border of the Irkutsk region and Yakutia, is still of great interest to some of researchers (geologists, crystallographers, geochemists, etc.). The outcrops of charoite-bearing rocks at the “Sirenevyi Kamen” deposit are noted both in the indigenous outcrops and in eluvial clatters [Bondarenko, 2009].

ReferencesBiryukov V.M., Berdnikov N.V., 1993. The paragenetic relation between charoite mineralization and alkali metasomatism. International Geology Review 35 (7), 585–602. https://doi.org/10.1080/00206819309465544.Biryukov V.M., Berdnikov N.V., 1993. The paragenetic relation between charoite mineralization and alkali metasomatism. International Geology Review 35 (7), 585–602. https://doi.org/10.1080/00206819309465544.Bondarenko N.V., 2009. The Geological and Structural Position and Genesis of the “Sirenevyi Kamen” Charoite Deposit. PhD Thesis (Geology and Mineralogy). Moscow, 150 p. (in Russian).Bondarenko N.V., 2009. The Geological and Structural Position and Genesis of the “Sirenevyi Kamen” Charoite Deposit. PhD Thesis (Geology and Mineralogy). Moscow, 150 p. (in Russian).Konev A.A., Vorobjev E.I., Lazebnik K.A., 1996. Mineralogy of the Murunsky Alkaline Massif. SIC UIGGM, Publishing House of SB RAS, Novosibirsk, 221 p. (in Russian).Konev A.A., Vorobjev E.I., Lazebnik K.A., 1996. Mineralogy of the Murunsky Alkaline Massif. SIC UIGGM, Publishing House of SB RAS, Novosibirsk, 221 p. (in Russian).Marchuk M.V., Medvedev V.Y., Ivanova L.A., Sokolova T.S., Danilov B.S., Gladkochub D.P., 2016. Charoite. Experimental studies. Geodynamics & Tectonophysics 7 (1), 105–118. https://doi.org/10.5800/GT-2016-7-1-0199.Marchuk M.V., Medvedev V.Y., Ivanova L.A., Sokolova T.S., Danilov B.S., Gladkochub D.P., 2016. Charoite. Experimental studies. Geodynamics & Tectonophysics 7 (1), 105–118. https://doi.org/10.5800/GT-2016-7-1-0199.Reguir E., 2002. Aspects of the Mineralogy of the Muran Alkaline Complex, Yakutia, Russia. National Library of Canada, 193 p.Reguir E., 2002. Aspects of the Mineralogy of the Muran Alkaline Complex, Yakutia, Russia. National Library of Canada, 193 p.Rozhdestvenskaya I., Mugnaioli E., Czank M., Depmeier W., Kolb U., Reinholdt A., Weirich T., 2010. The structure of charoite, (K,Sr,Ba,Mn)15-16 (Ca,Na)32[(Si70(O,OH)180)](OH,F)4*nH2O, solved by conventional and automated electron diffraction. Mineralogical Magazine 74 (1), 159–177. https://doi.org/10.1180/minmag.2010.074.1.159.Rozhdestvenskaya I., Mugnaioli E., Czank M., Depmeier W., Kolb U., Reinholdt A., Weirich T., 2010. The structure of charoite, (K,Sr,Ba,Mn)15-16 (Ca,Na)32[(Si70(O,OH)180)](OH,F)4*nH2O, solved by conventional and automated electron diffraction. Mineralogical Magazine 74 (1), 159–177. https://doi.org/10.1180/minmag.2010.074.1.159.Sokolova T.S., Danilov B.S., Dorogokupets P.I., 2016. Genetic features of charoite and tinaksite according to the data of high temperature decomposition reaction thermodynamic modeling. Proceedings of the Siberian Department of the Section of Earth Sciences of the RAEN. Geology, Exploration and Development of Mineral Deposits (1), 50–58 (in Russian).Sokolova T.S., Danilov B.S., Dorogokupets P.I., 2016. Genetic features of charoite and tinaksite according to the data of high temperature decomposition reaction thermodynamic modeling. Proceedings of the Siberian Department of the Section of Earth Sciences of the RAEN. Geology, Exploration and Development of Mineral Deposits (1), 50–58 (in Russian).Vorobjev E.I., 2008. Charoite. Geo Publishing House, Novosibirsk, 140 p. (in Russian).Vorobjev E.I., 2008. Charoite. Geo Publishing House, Novosibirsk, 140 p. (in Russian).

The authors declare that there are no conflicts of interest present.