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PALEOPROTEROZOIC CRYSTALLINE BASEMENT VOLHYNIAN PALEOZOIC RISING: CHARACTERISTICS OF GEOLOGICAL STRUCTURE AND HISTORY

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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Bibliographic Details
Main Author: MELNYCHUK, G.V.
Format: Article
Language:Ukrainian
Published: Institute of Geological Sciences, NAS of Ukraine 2013
Subjects:
paleoproterozoic
basement
Volyn Paleozoic rising
gneisses
amphibolites
granitoids
breaking structure
553.431(477.82)
палеопротерозой
фундамент
Волынское палеозойское поднятие
гнейсы
амфиболиты
гранитоиды
розрывные структуры
Волинське палеозойське підняття
гнейси
амфіболіти
гранітоїди
розривні структури
Online Access:http://geojournal.igs-nas.org.ua/article/view/139128
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http://geojournal.igs-nas.org.ua/article/view/139128

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