Publication details

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
Authors

FOJT Bohuslav PŘICHYSTAL Antonín

Year of publication 2015
Type Article in Periodical
Magazine / Source Acta Mus. Moraviae, Sci. geol.
MU Faculty or unit

Faculty of Science

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 %.

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