Fluoryt ze strefy korzeniowej złoża rud Zn-Pb kopalni „Bolesław"
Abstract
FLUORITE FROM ROOT ZONE OF ZN-PB ORE DEPOSIT OF THE „BOLESŁAW" MINE
Summary
In the Boleslaw mine area, three drillings have reached rocks of Upper Paleozoic basement. The encountered Permian conglomerates and Lower Carboniferous limestones are cut by ore veins. The paper mainly deals with those Permian conglomerate cutting veins which display fluorite mineralization. The veins are regarded as genetically related to Zn-Pb ores occurring in Mesozoic rocks. Up to the present, fluorite was not known from the Silesian-Cracow deposits.
Summary
In the Boleslaw mine area, three drillings have reached rocks of Upper Paleozoic basement. The encountered Permian conglomerates and Lower Carboniferous limestones are cut by ore veins. The paper mainly deals with those Permian conglomerate cutting veins which display fluorite mineralization. The veins are regarded as genetically related to Zn-Pb ores occurring in Mesozoic rocks. Up to the present, fluorite was not known from the Silesian-Cracow deposits.