Variability of copper mineralization in the Boundar Dolomite (Zechstein), Foresudetic Monocline, SW Poland: a statistical evaluation

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.

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