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Autor:
Valeriy V. Maslennikov, N. R. Ayupova, A. S. Tseluyko, A. V. Stepanov, Dmitry A. Artemyev, E. V. Belogub, A. V. Butnyakov, V. A. Kotlyarov
Publikováno v:
Geology of Ore Deposits. 63:79-86
Pyrite ores on the flanks of the Saum copper–zinc massive sulfide deposit are clastic sediments intensely transformed under conditions of acid diagenesis. Colusite in ores is confined to fine-grained pyrite clasts, which are rimmed by later small-c