Hydrotermální mineralizace

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Title in English Hydrothermal mineralisation
Authors

SLOBODNÍK Marek

Year of publication 2000
Type Chapter of a book
MU Faculty or unit

Faculty of Science

Citation
Description Calcite veins, which have been studied, originated during large migration of worm hydrothermal fluids (cca 8OC). The thickness of veins is up to several meters. The possibility of formation of caves by acting of that fluids is discussed.
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