The features of regional and contact metamorphism of cuprous sediments and catagenetic transformations of chromium sediments are considered. The conditions of formation of chromium-bearing glauconite are characterized. It is shown that ore formations (veins, skarns, hornblende, etc.) formed during regional and contact metamorphism can be used as search signs.
How to cite:
Bogdanov Y.V. Features of metamorphism of cuprous and chromitic sediments in the Olekmo-Vitim province // Journal of Mining Institute. 1997. Vol. 143. p. 101-107.
