Tektonika jednostki bocheńskiej i brzegu jednostki śląskiej między Rabą a Uszwicą

Abstract

Tectonic structure of the Bochnia unit and of the marginal part of the Silesian unit between the rivers Raba and Uszwica

Two overthrust Flysch covers stretch to the outer margin of the Carpathians between the Raba and Uszwica rivers (Figs 1-12). The Silesian unit is the inner one, while that of Bochnia (a part of the Sub-Silesian nappe) with Tortonian sediments, is the outer one. The stratigraphy of these two units has already been separately described (Olewicz 1968).