Abandoned quarry at the SW margin of Lišov granulite massif. Quarry opened pyroxenic granulite with intercalations of amphibolites and biotitic gneiss. Abundant aplites and pegmatites are connected mostly with paragneisses and contact of paragneisses with pyroxenic granulites. 4 major pegmatite bodies are known. Fissures in rocks are also filled with minerals of so-called alpine paragenesis.
References
Welser, P.: Minerály pegmatitů a alpské parageneze z Rudolfova u Českých Budějovic. Bulletin Mineralogicko-petrografického oddělení Národního muzea v Praze, 2002, roč. 10, s. 293-297.
Welser P., Zikeš J.: Magnetit z pegmatitu od Rudolfova u Č. Budějovic. Minerál, 2011, 19, 1, 12-15.
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