PALEOPROTEROZOIC CRYSTALLINE BASEMENT VOLHYNIAN PALEOZOIC RISING: CHARACTERISTICS OF GEOLOGICAL STRUCTURE AND HISTORY
Paleoproterozoic crystalline basement of Volyn Paleozoic rise is seen as a continuation of Centralbelorusska suture zone between Fennoscandia and Sarmatia. It is composed highlighted gneiss succession and girnitska association ortoamphibolites, as well as widespread for them Komarovska association...
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Datum: | 2013 |
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Format: | Artikel |
Sprache: | Ukrainian |
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Institute of Geological Sciences, NAS of Ukraine
2013
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Online Zugang: | http://geojournal.igs-nas.org.ua/article/view/139128 |
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Назва журналу: | Geological journal |