The point of view on two angular unconformities in the section of the Lower Carboniferous volcanosedimentary sequences of the northern Pamir is disproved.Two terrigenous sequences in contrast to one Beleuli sequence of shales are present in the Beleuli River basin.The first Carboniferous sequence conformably overlaps limestones with Serpukhovian goniatites and the second Permian sequence may be correlated with the Pshikharv Formation of shales from the western regions of the northern Pamir and contacts by the thrust Carboniferous rocks.
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