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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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The chemical composition of sphalerites from hydrothermal veins in rocks of the Lower Carboniferous of the Nízký Jeseník Upland and the block of Maleník (2004/1–2)Kučera, J., Slobodník, M., Sulovský, P, 2004: Chemické složení sfaleritů z hydrotermálních žil v horninách spodního karbonu Nízkého Jeseníku a kry Maleníku. – Acta Mus. Morav., Sci. Geol., 89, 1–2, 103–119 (with English summary)
The chemical composition of sphalerites from hydrothermal veins in rocks of the Lower Carboniferous of the Nízký Jeseník Upland and the block of Maleník
A chemical composition of sphalerites from polymetallic veins occurred in the Nízký Jeseník Upland and the block of Maleník have…
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