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Permo-Triassic stage of alkaline magmatism in the Vitim plateau (western Transbaikalia)
Authors:AG Doroshkevich  IA Izbrodin  MO Rampilov  GS Ripp  EI Lastochkin  VB Khubanov
Institution:1. Geological Institute, Siberian Branch of the Russian Academy of Sciences, ul. Sakh’yanovoi 6a, Ulan Ude, 670047, Russia;2. V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russiaa
Abstract:We present results of geochronological (40Ar-39Ar, U-Pb SHRIMP-II, and LA-ICP-MS) and geochemical studies of alkaline rocks of the Amalat, Sirikta, Tsipa, Pravyi Uligli, and Verkhnii Uligli massifs in the Vitim plateau (western Transbaikalia). The formation of the alkaline rocks and the accompanying albitization are dated at 261-242 Ma. The isotope inhomogeneity (?Nd(T) = + 8.4 to -1.7) of the alkaline rocks indicates the heterogeneous composition of the source of their material, having a depleted component, an enriched juvenile metasomatic fluid, and a crustal substrate.
Keywords:alkali and nepheline syenites  Permo-Triassic stage of magmatism  geochronological and isotope data  albitization  sources of material
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