Relation of hydrothermal mineralization with the content of some elements in the zones of dislocations

Abstract

All the most practically interesting deposits and ore occurrences within the South Slope of the Gissar Range are hydrothermal in nature and are localized within zones of discontinuous faults. In this connection, geochemical sampling of the material composing the zones of tectonic faults acquires extremely important significance, since it is obvious that the basic patterns of introduction or removal of elements in discontinuous faults can be used as geochemical criteria in the age subdivision of faults or in assessing their ore potential.

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