GEOLOGICAL CHARACTERISTICS OF THE ZIRABULAK ORE FIELD

Sultonov B.S.; Ishbobaev T.B.

doi:10.5281/zenodo.11551609

Sultonov B.S., Ishbobaev T.B.

Abstract. The article analyzes the results of previous studies of the Zirabulak ore field, and examines the data of recent years. The Zirabulak mining district covers the low-mountain uplifts of the Nurabad district of the same name in the southern part of Samarkand and, partially, Navoi regions. Geologically, it forms the northern flank of the Zeravshan-Alai structural-formation (metallogenic) zone, which is adjacent from the south to the Kuldzhuktau-Zeravshan regional zone of the west-northwestern strike. Based on the collected information and based on the geological conditions of ore content, stratigraphy, and magmatism of the region, the ore field deposits can be divided into two geological and industrial types: gold-quartz and gold-sulfide-quartz

Keywords: Zirabulak ore field, stratigraphy, ore content, deposits, geological and industrial type, gold-quartz.

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