Niektóre minerały i zjawiska kontaktowe z Podzamka koło Kłodzka

Olech Juskowiak

Abstract


SOME MINERALS AND CONTACT SYMPTOMS FROM PODZAMEK NEAR KŁODZKO (LOWER SILESIA)

At the boundary of the northwestern part of the Kłodzko-Złoty Stok massif and the Bardo structure, at Podzamek (Lower Silesia), there appear contact symptoms at the plane of contact of marble with a rock macroscopically resembling syenite. The following types of rock have been distinguished: 1) hedenbergite marbles, 2) vesuvianite skarns, 3) garnet rocks, 4) feldspathic-pyroxenic rocks with intercalations of amphibole rocks, 5) mixed rocks, monzonites - transition rocks to the syenites.

At the contact plane, these rocks form continuous zones of variable thickness; it is only the skarn which does not always appear and, in such instances, the marble contacts with the garnet rocks directly (Fig. 2).


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