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1966•International Geology ReviewRequires access

Characteristics of molybdenum stockwork deposit in eastern Transbaykalia

V.G. Kruglova, B. S. Chernov, A.G. Yevdokhin, Ye.S. Pastukhova

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Abstract

The type of this deposit is unusual for the region and the stock ore body lies outside the region's gold-molybdenum belt, in the area abounding in volcanic and subvolcanic rocks. The concentrically-zoned structured body is associated paragenetically with post-Upper Jurassic leucocratic granites; it appears to have been formed at shallow depths and at intermediate temperatures, as a member of the quartz-molybdenite-sericite formation, from neutral and weakly alkaline solutions. -- V.P. Sokoloff.

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What this paper is about

The type of this deposit is unusual for the region and the stock ore body lies outside the region's gold-molybdenum belt, in the area abounding in volcanic and subvolcanic rocks. The concentrically-zoned structured body is associated paragenetically with post-Upper Jurassic leucocratic granites; it appears to have been formed at shallow depths and at intermediate temperatures, as a member of the quartz-molybdenite-sericite formation, from neutral and weakly alkaline solutions. -- V.P. Sokoloff.

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Available abstract

The type of this deposit is unusual for the region and the stock ore body lies outside the region's gold-molybdenum belt, in the area abounding in volcanic and subvolcanic rocks. The concentrically-zoned structured body is associated paragenetically with post-Upper Jurassic leucocratic granites; it appears to have been formed at shallow depths and at intermediate temperatures, as a member of the quartz-molybdenite-sericite formation, from neutral and weakly alkaline solutions. -- V.P. Sokoloff.

Key concepts: Stockwork, Sericite, Molybdenite, Geology, Molybdenum, Geochemistry, Quartz, Volcanic rock

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