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CLEAVAGE, ITS NATURE AND FORECASTS WITHIN DONETS COALBED METHANE FIELD

This article observes conditions for occurrence of excessive cleavage areas within infolded perturbations of Donets Basin, their identification by mapping and analyzing the local structures (major) and by gradient maps. The article is also a review of conditions for forming of reservoir rock properties against the local anticlinal structures, which, being a part of the secondary folding, complicate the monoclinal bedding.  
 