phase of this complex, equal to 1.3. In the Dzhida region (Western Transbaykal) , granitoids of the Paleozoic...increases to 2. 4 in the granites of the Seletinsk massif, associated with the Ichkeul'mes copper deposit... In the granites of the Kyzyltau ( Kazakhstan) massif, this value increases to 11. 0, as a result of...Tantalum. K n = L I . In the granites of the Soktuy massif ( Eastern Transbaykal) ( Kuz'min et aL , 1972)... the value of K n is 2.4, and in the Kholderma massif, East Sayan (Morozov, 1972), 2. 7. The granites |