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Structure and Petrology of the Western Part of the Meliata Unit, West Carpathians
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Geolines
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January 1, 2006
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Copyright informationCopyright Institute of Geology 2006. Provided by ProQuest LLC. (Hide copyright information)
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The Meliata Unit with bluschist facies metamorphic rocks, exposed in the western part of the Gemericum, occurs in several localities around the StÃtnik and Nizná Slaná area. It forms tectonic slices overlying the early Paleozoic greenschist facies sedimentary and volcanic rocks with late Paleozoic metaconglomerates and also occurs beneath the unmetamorphosed or very low-grade metamorphosed Silica (Turna) Nappe formed mostly by limestones and dolomites. The Meliata and related rocks can be subdivided into two even three (upper, middle and lower) tectonic sheets. The most common rocks of the upper sheet are marbles with lenses of metabasite, different varieties of phyllites and rarely ...
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