Geotouristic sites of the Volhynian basalts

dc.contributor.authorDerevska, Kateryna
dc.contributor.authorShumlanskyi, Andrzej
dc.contributor.authorSolecki, Andrzej
dc.date.accessioned2020-02-25T11:00:42Z
dc.date.available2020-02-25T11:00:42Z
dc.date.issued2006
dc.description.abstractGetouristic sites illustrating geology of unique European occurrence of flood basalts similar to Siberian and Deccan Traps. Volhynian basalts being Precambrian (Vendian) in age are significantly older than the Siberian and Deccan ones, which formed at the end of Permian and Cretaceous respectively. In the case of Volhynian basalts additional point of interest is their native copper mineralization comparably with the legendary Lake Superior world's largest occurrence of native copper.en_US
dc.identifier.citationDerevska K. Geotouristic sites of the Volhynian basalts / Derevska K. I., Shumlanskyi V. O., Solecki A. T. // Geoeducational potential of southern and southwestern margin of the Ukrainian Craton / editors: I. M. Bubniak, A. T. Solecki, W. R. Sliwinski ; [Ivan Franko National University of L'viv, Faculty of Geology, University of Wrocław, Institute of Geological Sciences]. - Wrocław : Fundacja Ostoja, 2006. - P. 13-17.en_US
dc.identifier.urihttps://ekmair.ukma.edu.ua/handle/123456789/16984
dc.language.isoenen_US
dc.relation.sourceGeoeducational potential of southern and southwestern margin of the Ukrainian Cratonen_US
dc.statuspublished earlieren_US
dc.subjectgeologyen_US
dc.subjectVolhynian basaltsen_US
dc.subjectnative copperen_US
dc.subjectarticleen_US
dc.titleGeotouristic sites of the Volhynian basaltsen_US
dc.typeArticleen_US
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