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Geotouristic sites of the Volhynian basalts

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dc.contributor.author Derevska, Kateryna
dc.contributor.author Shumlanskyi, Andrzej
dc.contributor.author Solecki, Andrzej
dc.date.accessioned 2020-02-25T11:00:42Z
dc.date.available 2020-02-25T11:00:42Z
dc.date.issued 2006
dc.identifier.citation Derevska 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.uri http://ekmair.ukma.edu.ua/handle/123456789/16984
dc.description.abstract Getouristic 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.language.iso en en_US
dc.subject geology en_US
dc.subject Volhynian basalts en_US
dc.subject native copper en_US
dc.subject article en_US
dc.title Geotouristic sites of the Volhynian basalts en_US
dc.type Article en_US
dc.status published earlier en_US
dc.relation.source Geoeducational potential of southern and southwestern margin of the Ukrainian Craton en_US


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