Geneza karbońskich niecek na noworudzkim masywie gabrowo-diabazowym

Kazimierz Dziedzic

Abstract


GENESIS OF THE CARBONIFEROUS TROUGHS IN THE AREA OF THE NOW A RUDA GABBRO-DIABASE MASSIF

In the present article the author discusses the genesis of the depressions occurring in the area of the Nowa Ruda gabbro-diabase massif, which are filled up with the Carboniferous deposits. Moreover, an opinion on their erosional origin is given, too. They would correspond to the filled up river valleys formed at the Devonian period. The initial stages of the filling up process of these valleys, this the age of the oldest deposits occurring in these forms, fall on the decline of the Lower Carboniferous period.


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