Disappearing lignite seam in the Tomisławice opencast (Konin Basin, central Poland) – the case study based on field and borehole data

regarding a large mining problem. A narrow, so-called 'lignite-free'
zone occurs in the Tomisławice opencast in central Poland. This
surprising disappearance of an exploited lignite seam posed a threat
to the proper operation of a nearby Pątnów lignite-fired power plant.
Therefore, the Konin Lignite Mine carried out geological studies into
the 'lignite-free' area, as designated in the field.
During the investigation, it turned out that, in the 'lignite-free' zone,
there was, in fact, a continuous lignite seam, but it was at least 11 m
lower than the surrounding part of the 'Tomisławice' deposit. This
phenomenon can be explained in two ways. First, it could result from
greater peat-to-lignite compaction in the zone where the lignite seam
is at least twice thicker. Secondly, the zonal lowering of the lignite
seam could be caused by post-depositional tectonics, most likely of
Quaternary age. The latter hypothesis seems more probable at the
current stage of research.
Regardless of the reasons for such a large hypsometric lowering of
the exploited lignite seam, it is lost to the Konin Lignite Mine. Its
extraction is technically possible but would involve lowering the
mine water table in the cone depression by at least 11 m. Leaving
aside the formal and legal aspects, such action would be too costly
and, therefore, lignite from the examined 'lignite-free' zone will
remain as mining losses in the Tomisławice deposit.