Gorniy vestnik Uzbekistana


The Middle and South Tien Shan as orogenic regions with accompanying sharp changes in temperature and pressure (Koshmansai diatreme) are characterized by conditions for the formation of diamond manifestations. Prospects of Uzbekistan for radical manifestations of diamonds are assigned to the activated regions of the Archean (?) With manifestations of Lower Proterozoic eclogite-like formations with a complex of associated alpinotype ultrabasites, as well as alkaline intraplate basaltoids, K1.

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1. Uklonsky A.S. Mineralogy and geochemistry in Uzbekistan for 50 years of Soviet power // “Transactions of Tashkent State University”, - Tashkent, 1968, issue 337, -C.3-19. 2. Novgorodova M.I. Cubic silicon carbide in intergrowth with graphite and mummy diamond// DAN SSSR, 1984, vol. 227, No. 5, - S.1222-1227. 3. Efimov I.A. The most ancient breeds of Kazakhstan and Northern Kyrgyzstan // Avtoref.doct. Diss., - Alma-Ata: Academy of Sciences of the Kazakh SSR, 1972, -P.41. 4. Efimov I.A. Eclogites of gneiss-slatecomplexes of the Precambrian of the Kokchetav middle massif as tectonic inhabitants of the mantle of the Earth // "Problems of the geology of mineral deposits of Kazakhstan", - Almaty: OntiKazIMS, 1978.-S.89-102.



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