NATIVE GOLD FROM LODES AND PLACERS OF GLUKHARINY MINING CAMP, MAGADAN REGION

Authors

  • Glukhov A.N.
    N.A.Shilo Northeastern Complex Research Institute FEB RAS
    hD, Senior Researcher

  • Savva N.E.
    N.A.Shilo Northeastern Complex Research Institute FEB RAS
    h.D,

    Chief Researcher
  • Bulyakov G.H
    N.A.Shilo Northeastern Complex Research Institute FEB RAS
    hD

  • Fomina M.I
    N.A.Shilo Northeastern Complex Research Institute FEB RAS
    Senior Researcher
  • Biryukov A.A.
    N.A.Shilo Northeastern Complex Research Institute FEB RAS
    or researcher

Keywords:

native gold, mining camp, placer, lode source, mineral type, composition, metallogeny, evolution.

Abstract

Glukhariny gold mining camp is located in the central part of Kolyma terrane. It is composed of Nadezhda lode gold deposit, few gold ore occurrences and five gold placers. Known and explored gold mineralization is attributed to mesothermal granitoid-related and epithermal low-sulfidation types. Native gold from the gold placers is divided into five mineral types that correspond to lode sources of different type and age. Dependence of gold ore type and
mineralogy on host rock composition is shown. This is an example of the successive style of the Kolyma terrane metallogenic evolution.

Published

2020-10-09

How to Cite

Глухов Антон Николаевич, Савва Наталья Евгеньевна, Буляков Григорий Халитович, Фомина Марина Ивановна, & Бирюков Александр Александрович. (2020). NATIVE GOLD FROM LODES AND PLACERS OF GLUKHARINY MINING CAMP, MAGADAN REGION. Ores and Metals, (2). Retrieved from https://rm.tsnigri.ru/index.php/main/article/view/79

Issue

Section

Geology of ore deposits

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