Theoretical analysis of the role of groundwater flow in the genesis of stratabound ore deposits. 2. Quantitative results.

Abstract

The sensitivity to change in the numerical value of a given parameter in quantitative modelling of transport processes is assessed for a variety of hypothetical cross-sections. It is demonstrated that ground-water-flow systems could be responsible for conditions favourable to ore formation at ground-water discharge areas near the edge of a sedimentary basin. (Preceding abstract)-M.S.