
Study of the Carboniferous rocks eometamorphic alterations was carried out for the set of sections crossing the Main Anticline. It is defined that these alterations are derived from latent intrusive body as an additional source of heat. Palaeogeodynamical conditions appear strong variety along the Main Anticline; at the same time they show time stability from intrusion until the end of ore formation. Recommended area for detail golden ore prospecting appears to be the same with Mykhailivske golden ore occurrence in palaeogeodynamical conditions.
Постдіагенетичні зміни; карбон; Ольховатська площа; Донбас; рудоутворення, [553.068.1](477.6), Постдиагенетические изменения; карбон; Ольховатская площадь; Донбасс; рудообразование, Postdiagenetic change; Carboniferous; Olkhovatska area; Donbass; mineralization
Постдіагенетичні зміни; карбон; Ольховатська площа; Донбас; рудоутворення, [553.068.1](477.6), Постдиагенетические изменения; карбон; Ольховатская площадь; Донбасс; рудообразование, Postdiagenetic change; Carboniferous; Olkhovatska area; Donbass; mineralization
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