Abstract

This article presents the main geological factors of the location of mineralization in the Kuldzhuktau mountains. The paper notes the theory of the metamorphogenic-sedimentary genesis of gold ore mineralization, according to which, in the process of metamorphism, gold from the rocks of the amphibolite facies is carried out by fluids along tectonic shear zones and is deposited among the overlying rocks of the greenschist facies. The results of the study of thematic parameters of the relationship of gold mineralization with the structural elements of the region are described in more detail; they show that, among the variety of ore-controlling structural factors, meridional - transverse faults are of great information value. According to our field observations, it was established that the Taushan ore field includes a series of NNE and NE quartz veins.