Magnetic anomalies of mineralized cover of the Strzelin granitoids

Abstract

The crystalline schists from metamorphic cover of the Strzelin granitoids (Lower SiIesia) mineralized with iron and titanium oxides, reveal anomalies DZ which were analyzed by laboratory measurements of magnetic properties of these rocks. The analysis was supplemented by field and microscopic studies. It made possible to reconstruct the geological setting and distribution of mineralized schist zones, as well as to quantify the content of ore minerals.