Tabiiy fanlar

GEOCHEMICAL FEATURES OF GOLD MINERALITY OF THE SHOKHETAUS PROSPECTIVE AREA IN THE AUMINZATAU MOUNTAINS

Auminzatov, Shokhetov field, endogenous, oxidation zone, shales, tellurium, selenium, gold, antimony, silver, tungsten paragenesis, correlative connection, sulfosalt associations.

Authors

  • OLIMJON Qodirov X.M.Abdullaev nomidagi Geologiya va geofizaka instituti tayanch doktoranti, Uzbekistan
  • MAMATXAN Karabaev Geologiya fanlari universiteti professori, g.-m.f.d., Uzbekistan

In the article, the main gold mines of the Shokhetov field located in the southwestern part of the Auminzatov mountains and
information on the distribution properties of the accompanying elements is given. Dispersion characteristics of the main and
accompanying elements in the field in the mineralization processes, it is mainly gold-marginous, in addition to characterized by
the presence of gold-silver-sulfide-sulfosol geochemical paragenesis.