The pegmatites at Liverud and Gulliksrud ca. 5 kms E of Kongsberg, Øvre Eiker: A brief description of the pegmatites and their structural relationship to the adjacent banded gneisses is given. Some technical and economic implications are discussed. This type of pegmatite seems not to be promising for production of K-feldspar and quartz.
Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal