Stratigraphy of the Carboniferous deposits in northern part of the Góry Bardzkie, Sudetes.

Abstract

Conodonts occurring in gneissic breccias and conglomerates of the lower part of the Nowa Wieś formation point to the Visean age of these rocks. The overlying allodapic limestones were deposited in the Late Visean or Early Namurian. Most probably all the deposits of the Nowa Wieś formation represent the Upper Visean. Thus the overlying Srebrna Góra formation and the Zdanów melange complex are at least in part of the Namurian age.