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Paragenetická charakteristika železitých konkrecí z lokality "Zukalův kopec" na katastru obce Mokrá-Horákov
| Title in English | Paragenetic characterization of ferruginous concretions from the locality "Zukalův kopec" in the cadastral area of Mokrá-Horákov |
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| Authors | |
| Year of publication | 2015 |
| Type | Peer-reviewed scientific article |
| Magazine / Source | Acta Mus. Moraviae, Sci. geol. |
| MU Faculty or unit | |
| Citation | |
| Field | Geology and mineralogy |
| Keywords | Fe-concretions; geology; mineralogy; petrochemistry; Podolí Formation; Lower Carboniferous |
| Description | Origin of limonite concretions at the locality Zukalův kopec (cadastral area of the Mokrá-Horákov village) is connected with an intensive weathering of the specific calcareous Podolí Formation, probably in the warm climate of Tertiary. The concretions are formed by hadrated oxi-hydroxides of iron alternating with zones more or less rich in clastic components, i.e. especially in quartz and feldspars. The content of Fe2O3 is relatively high: about 50 - 60 weight %. |