CONDITIONS OF LOCALIZATION AND REGULARITIES OF LOCATION OF TUNGSTEN MINERALS ZERAVSHAN-ALAY METAL BELT (CENTRAL ASIA)

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Published Jan 21, 2021
https://doi.org/10.17605/OSF.IO/JRQ7N
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Vol. 6 No. 1 (2021): VOLUME 6 ISSUE 1

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O.T.Razikov
Chief Researcher, SI "IMR",State Committee for Geology of the Republic of Uzbekistan. Tashkent city, T. Shevchenko street, 11a

Abstract

This article examines the localization conditions and patterns of mineralization in the Zeravshan-Alai metallogenic belt. Described are ore-bearing rocks within the ore field of lime-skarn and magnesian-skarn formations, as well as skarnoids of both formations - magnesian and calcareous; near-skarn and near-ore-altered zones, including hornfelses, apogranite and containing various metasomatic formations. The paper describes four types of scheelite generations according to the formation conditions. The distribution of metasomatic zones of skarn ores with scheelite mineralization is natural.

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This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.

How to Cite
[1]
O.T.Razikov, “CONDITIONS OF LOCALIZATION AND REGULARITIES OF LOCATION OF TUNGSTEN MINERALS ZERAVSHAN-ALAY METAL BELT (CENTRAL ASIA)”, IEJRD - International Multidisciplinary Journal, vol. 6, no. 1, p. 8, Jan. 2021.
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