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Abstract

The Slovak Republic territory is from the abyssal geological structure point of view built by several tectonic mega units of various age. From the North it is the Proterozoic unit Brunia with overlying the Flysch; the next is the Klippen belt; than the partial tectonic crust unit of Cretaceous age (Tatricum, Veporicum, Gemericum) and superficial nappes system; and finally the South Alpine units (Pelső).In the areas of the Neogeneous development markedly hits into the deep structure influence of the lower crust and the upper mantle as a consequence of crust thinning and the ascent of the asthenolite what eventuated into creation of potential geothermal areas.

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/content/papers/10.3997/2214-4609-pdb.262.A07
2011-10-03
2024-04-27
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.262.A07
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