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Geochemistry and petrology of superpure quartzites from East Sayan Mountains, Russia

  • A. M. Fedorov
  • V. A. Makrygina
  • A. I. Nepomnyaschikh
  • A. P. Zhaboedov
  • A. V. Parshin
  • V. F. Posokhov
  • Yu. V. Sokolnikova
Original Article

Abstract

Quartzites are widespread within Earth’s lithosphere, but their highly pure varieties occur quite infrequently. With the development of alternative energy sources, including solar, and with increasing demand for high-purity quartz for optics, interest has risen in high-purity silicon-bearing materials. The quartzites discovered in the southeast part of the Eastern Sayan Mountains are particularly attractive for exploration in terms of their raw material quality and feasibility to be enriched. For this reason, their genesis also merits study. Available geochemical data show that chemogenic (d18O > 29.2‰) siliceous-carbonate sediments of the Irkut Formation are fairly pure (impurity elements < 800 ppm), and that half the impurities are easily removed carbonate components of the rock. Bedded quartzites remote from the intrusive granitoids and near-contact quartzites were recognized based on geochemical and petrographic data. Influenced by the Sumsunur granitoids, the near-contact quartzites originally contained > 0.9% impurities, but later, under the action of sliding slabs of ophiolite dynamothermal treatment reduced impurities to < 100 ppm, resulting in “superquartzites” (highly pure quartzites). The presence of only minor structural impurities is due to the enrichment capacity of superquartzites to 10.1 ppm (7.2 ppm under special conditions) of 10 elements: Fe, Al, Ti, Ca, Mg, Cu, Mn, Na, K, and Li.

Graphical Abstract

Keywords

High-purity quartz Superquartzite Gravitational sliding Dynamic metamorphism Recrystallization 

Notes

Acknowledgements

The work was performed under financial support of Integration Program No. 0341-2016-001 and Russian Foundation for Basic Research Projects 15-05-02772a and 18-05-00439a with research equipment isotope-geochemical studies at IGC SB RAS. We appreciate constructive comments from Skuzovatov S. Yu that significantly improved the quality of the paper. The authors thank sincerely Tatiana Bunaeva for preparation of the English version of the text.

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Copyright information

© Science Press, Institute of Geochemistry, CAS and Springer-Verlag GmbH Germany, part of Springer Nature 2018

Authors and Affiliations

  1. 1.A.P.Vinogradov Institute of Geochemistry SB RASIrkutskRussia
  2. 2.Irkutsk National Research Technical UniversityIrkutskRussia
  3. 3.Geological Institute SB RASUlan-UdeRussia
  4. 4.Irkutsk State UniversityIrkutskRussia
  5. 5.Irkutsk Scientific Center SB RASIrkutskRussia

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