The primary role of the fault zone in the formation and preservation of chrysotile-asbestos mineralization of the Bazhenov subtype, which can be attributed to deposits of near-fault metamorphism, has been established.
How to cite:
Efimov V.I., Barabanov V.P. Structure formation conditions of the Bazhenov chrysotile-asbestos deposit and regularities in the distribution of natural and industrial ore types // Journal of Mining Institute. 1997. Vol. 143. p. 63-69.
