ЕOMETAMORPHIC ALTERATIONS OF THE CARBONIFEROUS ROCKS AS AN INDICATOR OF ORE FORMATION EPOCH GEODYNAMICAL CONDITIONS WITHIN THE OLKHOVATSKA AREA DONBAS
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...
Збережено в:
| Дата: | 2012 |
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| Автори: | , , |
| Формат: | Стаття |
| Мова: | Ukrainian |
| Опубліковано: |
Institute of Geological Sciences, NAS of Ukraine
2012
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| Теми: | |
| Онлайн доступ: | http://geojournal.igs-nas.org.ua/article/view/139168 |
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| Назва журналу: | Geological journal |
Репозитарії
Geological journal| Резюме: | 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. |
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