Geotouristic sites of the Volhynian basalts

Derevska, Kateryna; Shumlanskyi, Andrzej; Solecki, Andrzej

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