Stosunek warstw żaclerskich do gnejsów sowiogórskich między Głuszycą a Sierpnicą w Sudetach Środkowych

Wojciech Grocholski


Relation of the Żacler beds to the Sowie Góry gneisses in central Sudeten Mts.

Contact of the Sowie Góry archaic gneisses with the sedimentary rocks of the Intra-Sudetic Basin between Głuszyca and Sierpnica has a tectonic character. A recurrently rejuvenated dislocation zone, in which mylonites are one of the elements, occurs on the boundary of these two series.

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