Abstract
The suggested classification of organogenic deposits of the Lower Famennian in the Pripyat Trough was developed on the grounds of available classifications and data of geological (lithologic, palaeontological, palaeoecological) investigations carried out in the region. This classification provides an opportunity to identify unambiguously and to correlate these genetically similar deposits, their groups, types and kinds (forms) widespread in many palaeobasins throughout the world, especially those promising for various mineral occurrences.
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