Bukantov va Auminzatov toglari oltin-nodirmetalli, oltin-kumushli konlarida majmuasi, mineral tarkibi, hosil bolish sharoitiga qarab farq qiluvchi metasomaik tog jinslari ajratilgan. Metasomatitlarning alohida turlari bilan ularga xos bolgan madanlashuv bogliqligi ushbu hosilalaming yagona mineral hosil bolish jarayoni bosqichlarining tadrigiy rivojlanishini aks etdiradi. Nodirmetalli madanlashuv magniyli hamda ohakli skamlardan keyin, greyzenli, qvarts-dala shpatli, aposkarnli metasomatitlar bilan bir paytda vyjydga kelgan. Ketma-ket rivojlanuvchi propilit, berezit, eysit va argillizit madan atrofi dzgargan tog jinslari bilan oltin-vismut-telluridli, oltin-margimushli, kopsulfidli-telluridli va oltin-sulfatuzli madanlashuv bosqichlari bogliq ekanligi aniqlangan.
Tayanch iboralar: Bukantov, Auminzatov, metasomatitlar, mineral tarkibi, ketma-ketligi, mineral hosil bolish jarayoni, bosqichlari, munosabatlari, madanlashuv, nodirmetalli, oltinli, bir paytda, ketma-ket rivojlanuvchi.
Highlighted metasomatic rocks of gold and gold-silver-rare-metal deposits and mountains Bukantau Auminzatau characterized by their complex, mineral composition and characteristics of the formation. With certain types metasomatitov associated respective steps mineralization which are typomorphic their features and characteristics reflect the evolution stages and a single system of the mineral. Rare metal (and gold) mineralization both magnesia and lime in skams imposed - skamy are favorable environment for mineralization. Greisen, quartz-feldspar, aposkamovye Metasomatites are synchronous Wallrock changes, and they are associated with rare metal mineralization, with successively formed propylites, beresites, eysitami and argillisites conjugate of gold-bismuth-telluride,-arsenic gold, polysulfide-telluride and gold-sulphosalt step mineralization.
Key words: Bukantau, Auminzatau, metasomatic, mineral composition, zonality, mineral forming step, interrelation, mineralization, rare metal, gold, synchronical, connect.
