THE RARE METALS AND ORIGIN OF THE LITHIUM-FLUORINE GRANITES OF THE UKRAINIAN SHIELD
According to the resulns of research features of the distribution of chemical elements in the lithium-fluorine grantites of the Ukrainian Shield by geological and mathematical methods approved by the vast majority of the lithitum-fluorine granites formed as a result of metasomatic transformation of...
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/139192 |
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| Назва журналу: | Geological journal |
Репозитарії
Geological journal| Резюме: | According to the resulns of research features of the distribution of chemical elements in the lithium-fluorine grantites of the Ukrainian Shield by geological and mathematical methods approved by the vast majority of the lithitum-fluorine granites formed as a result of metasomatic transformation of granite standard geochemical type, which were substratum rocks for the first. Since Omelyaniv and Ignatpol granites rapakivi type of Korosten comtplex are transitive formations to the lithium-fluorine geochemical type granites, in a field of their development it is possible to expect revealing cutting-bodys of zinnwaldite-albite-microcline granites, which are productive for rare-metal mineralization. Also argued, why granites of Kamennye Mogily complex, which on geochemical parameters belong to the same geochemical type, are less interesting to the geologists in terms of their practical significance. |
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