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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 valley.In 2003-2004 structural tectonic evaluation of the gypsum anhydrite deposit of afárka was done in the framework of geological prospection etape. The results show that the mutual structural tectonic position of the Upper Permian Nová Ves formation and Lower Triassic formations (Silica Nappe of the Silicicum tectonic unit) is unconformable.
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 valley.In 2003-2004 structural tectonic evaluation of the gypsum anhydrite deposit of afárka was done in the framework of geological prospection etape. The results show that the mutual structural tectonic position of the Upper Permian Nová Ves formation and Lower Triassic formations (Silica Nappe of the Silicicum tectonic unit) is unconformable.
Structural tectonic analysis of afárka gypsum quarry, Spi-Gemerské Rudohorie Mts. (Western Carpathians)
Sasvári Tibor (author)
2004
Article (Journal)
Electronic Resource
Unknown
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