Supergenní mineralizace z haldy šachty č. 16 Příbram - Háje

Pages

43-55

Citation

PAVLÍČEK, Radim, GOLIÁŠ, Viktor, ŠKÁCHA, Pavel, ČEJKA, Jiří, SEJKORA, Jiří, PLÁŠIL, Jakub a HOFMAN, Petr. Supergenní mineralizace z haldy šachty č. 16 Příbram - Háje. Bulletin mineralogicko-petrologického oddělení Národního muzea v Praze. Prague: National Museum, 2008, 16(1), 43-55. ISSN 1211-0329 (print), 1804-6495 (online). Also available from: https://publikace.nm.cz/en/periodicals/bmpholnrhmvp/16-1/supergenni-mineralizace-z-haldy-sachty-c-16-pribram-haje

Bulletin mineralogicko-petrologického oddělení Národního muzea v Praze | 2008/16/1

Uranium supergene minerals from Háje near Příbram were formed during ca. 30 years storage on a mining dump of the shaft No.16. Following minerals were there identified: brochantite, cerrusite, fourmarierite, liebigite, metazeunerite, natrozippeite, pharmacolite, uranopilite, uranospinite, schoepite, schröckingerite, tyuyamunite and znucalite. New data for fourmarierite (XRD, IR), metazeunerite (XRD), natrozippeite (XRD), pharmacolite (XRD), schoepite (XRD, IR) and znucalite (XRD, IR) are given. The origin of described minerals is discussed. All mineral phases found represent recent or sub-recent alteration products of primary mineralization: uraninite, antraxolite and base metal sulphides, which are highly inhomogenously distributed in the dump material. Therefore the occurrences of supergene mineralization are locally restrained.

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