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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
Date:	2013
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)
Online Access:	http://geojournal.igs-nas.org.ua/article/view/139128
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Journal Title:	Geological journal

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Geological journal

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