FAR EASTERN ILMENITE AND MAGNETITE MAGMATIC ROCKS
Аннотация
Ilmenite magmatism is characteristic of ore deposits, and it is absent in magnetite-series rocks. Modern methods in Redox conditions mapping can be used to identify promising areas for tin deposits prospecting.
The redox – conditions maps were made, and it was determined the boundaries of ilmenite and magnetite magmatism for the Far Eastern magmatic structures of Eastern Yakutia, the Mongol-Okhotsk western part , and Sikhote-Alin orogenic belts.
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Литература
Mishin L.F., Kirillova G.L., Merkulova T.V., Konovalova E.A. Postcollision Magmatism of Western Sector of the Mongol–Okhotsk Orogenic Belt: Oxidation Conditions and Metallogenic Zoning. Tikhookeanskaya geologiya, 2019, vol. 38, no. 4, pp. 3–13. DOI: 10.1134/S1819714019040067 (In Russ.).
Mishin L.F., Konovalova E.A., Taltykin Yu.V., Krutikova V.O., Dobkin S.N., Yurchenko Yu.Yu., Shtareva A.V. Redox conditions and related geochemical and metallogenic zonation of magmatic rocks of the Sikhote Alin Orogenic Belt. Tikhookeanskaya geologiya, 2020, vol. 39, no. 3, pp. 51–67. DOI: 10.1134/S1819714020030057 (In Russ.).
Taltykin Yu.V., Mishin L.F., Konovalova E.A. Redox background in the earth’s crust of the Sikhote-Alin orogenic belt in crystallization of Cretaceous-Paleogene magmatites: connection with geodynamics. Vestnik SVNTs DVO RAN, 2020, no. 4, pp. 24–38. DOI: 10.34078/1814-0998-2020-4-24-38 (In Russ.).
Ishihara S. Granitoid Series and Mineralization in the Circum-Pacifc Phanerozoic Granitic Belts. Resource Geology, 1998, vol. 48, no. 4, pp. 219–224.
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