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MAIN TYPES OF GOLD DEPOSITS OF THE EASTERN KAZAKHSTAN

Marina Mizernaya, B. Dyachkov, O. Kusmina, A. Mizerny, Tatyana Oitseva

First published: 2017-06-20https://doi.org/10.5593/sgem2017/11/s01.038View metrics

Abstract

The Bolshoi Altay (BA) located in the north-west part of Central Asian mobile belt on territory of the East Kazakhstan. The geological structures of the BA include Rudniy Altay, Kalba-Narym (in the north-west), Zharma-Saur, and neighbouring regions of Russia and China and, was formed in the Hercynian time in the process of collision of Kazakhstan and Siberian lithosphere plates and degradation of Irtysh-Zaisan paleo ocean. Regional and local criteria for forecasting of gold ore deposits of the BA have been developed, their age position has been ascertained and their relations with certain geological formations have been determined. The Zaisan collision zone (with an extension of more than 1000 km and width of 20-40 km) is of ore controlling importance. It was formed as a result of concussion and turning of lithosphere plates. The zone corresponds to the East-Kazakhstan gold ore belt of regional ranging. Within this zone there are more than 450 deposits and ore occurrences of gold including the unique Bakyrchik deposit. The flanks of the gold ore belt can be traced to Russia and China, its perspectives are underexplored.

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  • CrossRef - Citation Indexes: 5
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Publication details

Title
MAIN TYPES OF GOLD DEPOSITS OF THE EASTERN KAZAKHSTAN
Authors
Marina Mizernaya, B. Dyachkov, O. Kusmina, A. Mizerny, Tatyana Oitseva
Proceedings
SGEM International Multidisciplinary Scientific GeoConference EXPO Proceedings; 17th International Multidisciplinary Scientific GeoConference SGEM2017, Science and Technologies in Geology, Exploration and Mining
Publisher
STEF92 Technology
Year
2017
Pages
299-306
SWS Citekey
Mizernaya20171299306
ISSN
1314-2704
ISBN
978-619-7105-98-8
Language
en
Publication type
Conference Paper
Keywords
metallogenic specializationore beltgold depositsKazakhstan
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Number of times cited according to Crossref: 5

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