Budowa geologiczna antykliny Wojszyc

Sylwester Marek

Abstract


GEOLOGICAL STRUCTURE OF WOJSZYCE ANTICLINE

The Wojszyce anticline is situated in the eastern part of the middle section·of the so-called Kutno elevation (Fig. 1). This anticline is probably a salt structure where, however, the Zechstein salt mass failed to pierce the superimposed geological formations, but caused their upheaval in the form of an anticline.


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