The distribution of the Cu mineralization associated with the Vendian red beds is discussed. Mineralization is restricted to the zones transitional from red beds to the under- and overlying rocks. Rich ore deposits are associated with carbonaceous matter in the permeable, coarse, clastic red beds near the palaeo-uplift.-R.E.S.
CITATION STYLE
Gablina, I. F. (1986). Genetic types of copper mineralization in the Igarka area, west of the Siberian platform. Geology and Metallogeny of Copper Deposits, 524–539. https://doi.org/10.1007/978-3-642-70902-9_38
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