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                                       Details for article 10 of 15 found articles
 
 
  Structural – tectonic analysis of Šafárka gypsum quarry, Spiš-Gemerské Rudohorie Mts. (Western Carpathians)
 
 
Title: Structural – tectonic analysis of Šafárka gypsum quarry, Spiš-Gemerské Rudohorie Mts. (Western Carpathians)
Author: Sasvári Tibor
Appeared in: Acta Montanistica Slovaka
Paging: Volume 9 (2004) nr. 2 pages 134-140
Year: 2004
Contents: In the northern part of the Spiš-Gemerské Rudohorie Mts. evaporite facies occurs in the Nová Ves Formation. The evaporite horizon was described at the level of zero storey at the Spišská Nová Ves – Nová Štôlòa deposit. The horizon is open by a strip pit Šafárka and also in the NW part of the Markušovce valley.In 2003-2004 structural – tectonic evaluation of the gypsum – anhydrite deposit of Šafárka 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.
Publisher: Technical University of Kosice, the Faculty of Mining, Ecolo
Source file: Elektronische Wetenschappelijke Tijdschriften
 
 

                             Details for article 10 of 15 found articles
 
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