These deposits are usually formed in sea-floor depressions, preceded by stratification of sea-water into oxidizing and reducing zones. Pyritic bodies are formed in two stages: primary sedimentation takes place in thermodynamic disequilibrium conditions but the final form of the deposit is determined by diagenetic processes buffered within narrow ranges. -R.E.S.
CITATION STYLE
Tvalchrelidze, A. G. (1986). Physico-chemical conditions of base metal sulphide ore formation. Geology and Metallogeny of Copper Deposits, 358–369. https://doi.org/10.1007/978-3-642-70902-9_26
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