Tidal flat and flood-plain . deposits in the Lower Devonian of the western Lublin Uplands (after the boreholes Pionki 1 and Pionki 4)

Henryk Łobanowski, Teresa Przybyłowicz


Fades analysis of the Lower Devonian deposits recorded fu the boreholes Pionki 1 and Pionki 4 located in the western Lublin Uplands, between the Holy Cross Mts and the south-western margin of the East-European platform, permits a recognition of marine, tidal-flat, and flood-plain environments. The accumulated clastic material derived from the East-European platform.

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