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Structural tectonic analysis of afárka gypsum quarry, Spi-Gemerské Rudohorie Mts. (Western Carpathians)

In the northern part of the Spi-Gemerské Rudohorie Mts. evaporite facies occurs in the Nová Ves Formation. The evaporite horizon was described at the level of zero storey at the Spiská Nová Ves Nová tôlòa deposit. The horizon is open by a strip pit afárka and also in the NW part of the Markuovce va...

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Kaydedildi:
Detaylı Bibliyografya
Yazar: Sasvári Tibor
Materyal Türü: Artigo
Dil:Inglês
Baskı/Yayın Bilgisi: Technical University of Kosice 2004-06-01
Seri Bilgileri:Acta Montanistica Slovaca
Konular:
Online Erişim:http://actamont.tuke.sk/pdf/2004/n2/14sasvari.pdf
Etiketler: Etiketle
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