Quartz Concentrates Based on Compact Quartzite


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This paper presents a study of a variety of quartz material from East Sayan: compact quartzite from the Oka–Urik block. We have investigated the texture and structure of quartz and mineral and fluid inclusions in it. It has been shown that the fluid inclusions are located mainly in the quartz grains and that the major salt component in the fluid inclusions is sodium. In the case of compact quartz, we have proposed a process for the preparation of extrapure quartz concentrates. A distinctive feature of the process is high-temperature precalcination of quartz grit prior to chemical enrichment, which makes it possible to open the fluid inclusions and remove sodium.

作者简介

A. Nepomnyashchikh

Vinogradov Institute of Geochemistry, Siberian Branch; Irkutsk Scientific Center, Siberian Branch

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Email: ainep@igc.irk.ru
俄罗斯联邦, ul. Favorskogo 1a, Irkutsk, 664033; ul. Lermontova 134, Irkutsk, 664033

M. Volkova

Vinogradov Institute of Geochemistry, Siberian Branch; Irkutsk Scientific Center, Siberian Branch

Email: ainep@igc.irk.ru
俄罗斯联邦, ul. Favorskogo 1a, Irkutsk, 664033; ul. Lermontova 134, Irkutsk, 664033

A. Zhaboedov

Vinogradov Institute of Geochemistry, Siberian Branch; Irkutsk Scientific Center, Siberian Branch

Email: ainep@igc.irk.ru
俄罗斯联邦, ul. Favorskogo 1a, Irkutsk, 664033; ul. Lermontova 134, Irkutsk, 664033

A. Fedorov

Vinogradov Institute of Geochemistry, Siberian Branch; Irkutsk Scientific Center, Siberian Branch

Email: ainep@igc.irk.ru
俄罗斯联邦, ul. Favorskogo 1a, Irkutsk, 664033; ul. Lermontova 134, Irkutsk, 664033

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