Czerwony spągowiec w otoczeniu bloku przedsudeckiego
Abstract
ROTLIEGENDES IN THE VICINITY OF THE FORE-SUDETIC BLOCK
Summary
The author argues that the Zielona Góra Syncline should be distinguished within the south-western part of the Fore-Sudetic Monocline. He points to considerable similarities in the development of the sediments of the particular cycles of the Rotliegendes in the North-Sudetic Depression and in the Zielona Góra Syncline. A comparison between these deposite is presented. The author emphasizes the influence of theSaalephase in the development of Lower Permian deposits in this region.
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