New Kaolin-Bearing Province of Russia in the Southern Part of the Voronezh Anteclise


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Abstract

The lithofacies analysis of the Mamon sequence showed that secondary kaolin deposits, forming a new kaolin-bearing province in the southern part of the Voronezh Anteclise, are associated with a complex of deluvial–proluvial, lacustrine–boggy, and floodplain–oxbow deposits. The main ore minerals are kaolinite, quartz and secondary iron oxides, and gibbsite. The presence of both terrigenous and authigenic kaolinite was revealed. An organic substance played an important role in the formation of the latter, as well as gibbsite.

About the authors

A. D. Savko

Voronezh State University

Email: boeva@igem.ru
Russian Federation, Voronezh, 394018

V. M. Novikov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences

Email: boeva@igem.ru
Russian Federation, Moscow, 119017

N. M. Boeva

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences

Author for correspondence.
Email: boeva@igem.ru
Russian Federation, Moscow, 119017

A. V. Krainov

Voronezh State University

Email: boeva@igem.ru
Russian Federation, Voronezh, 394018

A. V. Milash

Voronezh State University

Email: boeva@igem.ru
Russian Federation, Voronezh, 394018

E. A. Zhegallo

Borissiak Paleontological Institute, Russian Academy of Sciences

Email: boeva@igem.ru
Russian Federation, Moscow, 117997

M. Yu. Ovchinnikova

Voronezh State University

Email: boeva@igem.ru
Russian Federation, Voronezh, 394018

N. S. Bortnikov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences

Email: boeva@igem.ru
Russian Federation, Moscow, 119017

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