Abstract
Eight lithological sequences are recognized among the Mesozoic sediments that cover the Carboniferous coal-bearing formation. Those are (upward): terrigenous, terrigenous-carbonate, Upper Jurassic carbonate, lower sand, upper sand, limestone, lower marl, and upper marl of the Upper Cretaceous. The terrigenous Jurassic and sand Lower Cretaceous sequences influenced most negatively the conditions of coal mining. The basin has been zoned on the influence of Mesozoic sediments over geological and mining conditions of coal recovery.
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