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Replacement of hydrothermal chalcopyrite by bornite and Cu sulfides from the quarry of the cement factory Hranice: a hypogene minerogenetic process? (2026/1)Dolníček, Z., Kotlánová Krejčí, M., Koutňák, R., 2026: Zatlačování hydrotermálního chalkopyritu bornitem a Cu sulfidy z lomu cementárny Hranice: hypogenní minerogenetický proces?. – Acta Mus. Morav., Sci. Geol., 111, 1, 3–22 (with English summary)
Replacement of hydrothermal chalcopyrite by bornite and Cu sulfides from the quarry of the cement factory Hranice: a hypogene minerogenetic process?
A new occurrence of a Cu-mineralization hosted by a post-Variscan calcite vein was found in the limestone quarry of the cement factory at the…
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Mineralogy and formation conditions of the hydrothermal calcite-barite-chlorite mineralization from Adamov (Brno massif) (2005/1–2)Dolníček, Z., 2005: Mineralogie a podmínky vzniku hydrotermální kalcit-baryt-chloritové mineralizace od Adamova (brněnský masiv). - Acta Mus. Moraviae, Sci. Geol., 90, 1-2, 109-120 (with English summary)
Mineralogy and formation conditions of the hydrothermal calcite-barite-chlorite mineralization from Adamov (Brno massif)
Calcite-barite-chlorite mineralization from Adamov hosted by Neoproterozoic granodiorites of the Brno massif has been studied using EDX microanalyses, fluid inclusion microthermometry…
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