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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Bibliographische Detailangaben
Datum:2013
1. Verfasser: MELNYCHUK, G.V.
Format: Artikel
Sprache:Ukrainian
Veröffentlicht: 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

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Geological journal