Geologie paleozoika CHKO Litovelské Pomoraví, střední Morava = Geology of Paleozoic of the Litovelské Pomoraví Protected Area, Central Moravia
The area of interest represents isolated outcrops situated between the Jeseníky and Drahany part of the Paleozoic Moravian-Silesian basin. Petrological and mineralogical study of graywackes, namely of translucent heavymineralassemblages show similarities with both Nízký Jeseník and Drahany psammitic Lower Carboniferous material. Thus the idea of one continuos … full description
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Bibliographic Details
- Main Author
- Document Type
- Articles
- Physical Description
- il.
- Published in
- Acta Musei Moraviae. Scientiae geologicae. -- ISSN 1211-8796. -- Roč. 82, (1997), s. 93-103
- Subjects
MARC
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245 | 1 | 0 | |a Geologie paleozoika CHKO Litovelské Pomoraví, střední Morava = |b Geology of Paleozoic of the Litovelské Pomoraví Protected Area, Central Moravia / |c Jiří Otava |
246 | 3 | 1 | |a Geology of Paleozoic of the Litovelské Pomoraví Protected Area, Central Moravia |
300 | |b il. | ||
520 | |a The area of interest represents isolated outcrops situated between the Jeseníky and Drahany part of the Paleozoic Moravian-Silesian basin. Petrological and mineralogical study of graywackes, namely of translucent heavymineralassemblages show similarities with both Nízký Jeseník and Drahany psammitic Lower Carboniferous material. Thus the idea of one continuos large Lower Carboniferous basin is supported. The contemporary separated pattern is theresultof later displacement along | ||
520 | |a The the tectonic zone of Haná (the continuation of the Elbe lineament) | ||
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773 | 0 | |t Acta Musei Moraviae. Scientiae geologicae |x 1211-8796 |g Roč. 82, (1997), s. 93-103 |q 82 |9 1997 | |
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