Nodule vápenatosilikátovych hornin v poličském krystaliniku a jejich litologicky význam

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Acta Mus. Moraviae, Sci. Geol. 90 (2005), vydání 1–2, stránky 121-146
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The nodules of calc-silicate rocks from Polička crystalline unit and their lithologic significance

The nodules of calc-silicate rocks from several localities in the Polička crystalline complex were studied using various mineralogical and petrological methods. Nodules are enclosed in the biotite to muscovite-biotite gneises and located in 2 km thick zones situated concordantly with the main foliation of the Polička crystalline complex from NW to SE. These rocks are a product of the metamorphism predominantly calcareous concretions under amphibolite facies conditions and mineral assemblage indicated very low XCO2.

Kontakt:

David Buriánek, Czech Geological Survey, Leitnerova 22, 658 59, Brno, Czech Republic, burianek@cgu.cz

Citace
Buriánek, D., 2005: Nodule vápenatosilikátovych hornin v poličském krystaliniku a jejich litologicky význam. - Acta Musei Moraviae, Sci. Geol., 90, 1-2, 121-146 (with English summary)
ISSN: 1211–8796