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Age and origin of the Kitoi sillimanite schist deposit, eastern Siberia
Age and origin of the Kitoi sillimanite schist deposit, eastern Siberia
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Age and origin of the Kitoi sillimanite schist deposit, eastern Siberia
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Age and origin of the Kitoi sillimanite schist deposit, eastern Siberia
Age and origin of the Kitoi sillimanite schist deposit, eastern Siberia
Journal Article

Age and origin of the Kitoi sillimanite schist deposit, eastern Siberia

2010
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Overview
The Kitoi sillimanite schist deposit is located on the left side of the Kitoi River within the Sayan (Sharyzhalgai) marginal uplift of the Siberian Platform basement. In this district, sillimanite was described for the first time in 1951. In 1958, a geological crew under the supervision of I. M. Shirobokov revealed a significant amount of sillimanite as a result of geological survey and after lengthy exploration, 1959-1968, it was recognized as the largest alumina deposit in Eastern Siberia. The total reserves of the deposit are a few hundred million tons with sillimanite grade more than 20%.
Publisher
SP MAIK Nauka/Interperiodica,Springer,Springer Nature B.V