Prediction Criteria Based on Mineralogical and Geochemical Features of Tin Ore Occurrence (East Kazakhstan)

New research results of the Yubileyny Oktyabr rare metal ore occurrence are being considered. The Yubileyny Oktyabr ore occurrence is located in West Kalba metallogenic zone, in the southern exocontact of Delbegetey granite massif. According to the new results of the study, the ore occurrence is compared with a non-conventional type of stannum-bearing mineralized zones, associating with small intrusions and dikes of collision type Kunush complex (C3) [1]. A distinctive feature of the deposit is that the stannum ore of hydrothermal-metasomatic type is superimposed on the porphyry intrusions C3 and the host sedimentary rocks of Bukon formation (C2), and genetically associated with granites of Delbegetey complex (P1), in comparison with similar rare-metal deposits (the Karasu, the Cherdoyak, the Novaya Tochka, the Rzhavaya Sopka, etc.) [2]. The research goal is to show mineralogical and geochemical features based on a systematic analysis of materials from previous studies and new results. To develop predictive and search criteria for evaluating similar objects. For further use of these data during deep geological and mineragenic mapping of the territory of East Kazakhstan