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


Дәйексөз келтіру

Толық мәтін

Ашық рұқсат Ашық рұқсат
Рұқсат жабық Рұқсат берілді
Рұқсат жабық Тек жазылушылар үшін

Аннотация

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.

Авторлар туралы

A. Savko

Voronezh State University

Email: boeva@igem.ru
Ресей, Voronezh, 394018

V. Novikov

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

Email: boeva@igem.ru
Ресей, Moscow, 119017

N. Boeva

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

Хат алмасуға жауапты Автор.
Email: boeva@igem.ru
Ресей, Moscow, 119017

A. Krainov

Voronezh State University

Email: boeva@igem.ru
Ресей, Voronezh, 394018

A. Milash

Voronezh State University

Email: boeva@igem.ru
Ресей, Voronezh, 394018

E. Zhegallo

Borissiak Paleontological Institute, Russian Academy of Sciences

Email: boeva@igem.ru
Ресей, Moscow, 117997

M. Ovchinnikova

Voronezh State University

Email: boeva@igem.ru
Ресей, Voronezh, 394018

N. Bortnikov

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

Email: boeva@igem.ru
Ресей, Moscow, 119017

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