The Problem of Dynamometamorphic Transformations of Rocks and Ores of the Upper Part of the Ridder-SokoFnoe Deposit (Rudnyi Altai)

摘要

The Ridder-Sokol'noe polymetallic deposit is located in the northern part of the Leninogorskoe ore field within the zone of the Semipalatinsk-Leni-nogorsk sublatitudinal regional fault in relatively poorly deformed layered series of the arch part of the anticline structure (Fig. 1) and is represented by ore bodies located at various hypsometric levels in different tectonic blocks [1-4 and others].