Facje młodoczwartorzędowych aluwiów dorzecza środkowego Bugu

Jan Rzechowski

Abstract


FACIES OF LATE QUATERNARY ALLUVIA IN THE MIDDLE BUG RIVER BASIN

The present author takes a try at :comparing the macro-structural features of various alluvial facies with their granular and mineral properties. Three alluvial series differing in their age are found within the area under study (Fig. 1): Holocene series (H), younger Pleistocene series (P1) and older Pleistocene series (P2). The following facies have been distinguished in the series mentioned above: flood facies, channel facies and dead channel facies.


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