SUMMARY
North-easteI"ll regioos of Poland are very
poor
in
solid mdneral Ifuel mate1"ials. Peat is the only ma-terial of that type occurring here, sometimes even in large aIDOWlts. Geologi<:a1 structure of this
IP8rt
of Poland precludes occurrence of black coal de-posits, as the Paleozoic sedimentary cover overlying the Precambrian Platform is devoid of Carboniferous formation. There remains a possibility of occurrence of
brown
coals
in
Keuper and Liassic fonnations, which has not been confirmed by the up-to-date studies, or in the Tertiary formation.With these premises
in
mind, the present author conducted systematic geologiJcal studies of theTer-tiary formation
in
the north-eastern Poland. The results of these studies are glVE'.nin
the presentpaper.
PE3IOME,
PaiiOHDI ceBepo-Boc'ro'iUoti nom.11IH lSe~t
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Tpem'lHhIe OTJIOlKeBHJI.
HCXOP;R M3 STMX npcp;nOCLIJIDK, asrop npoaeJI p;e-TaJIbHoe M3Y'lel{Me TpeTH"fHLIX O'l'JIOlKeuMf.i: ceBepo-BO-CTO"fIlOA nom.um. B CT8TLe M3JlOlKeHhI pe3YJIb'l'8'l'1>I STMX HCCJIep;OBaHM.
