Variability of copper mineralization in the Boundar Dolomite (Zechstein), Foresudetic Monocline, SW Poland: a statistical evaluation
Authors
Barbara Namysłowska-Wilczyńska
Abstract
Zmienność mineralizacji miedziowej w dolomicie granicznym (cechsztyn, monoklina przedsudecka) w świetle badań statystycznych
Cu-grade and thickncss variability of the Boundary Dolomite (Zechstein of the Foresudetic Monocline) was studied by means of distribution shape analysis, correlation and surface trend analysis. The results indicate that the copper mineralization in the Boundary Dolomite has an infiltralional character. This process was accompanied by displacement of ore-bearing solutions from the overlying Kupferschiefer into the Boundary Dolomite.
