The supergene mineral association with brandholzite from Pernek, Malé Karpaty Mountains, Slovak Republic

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00023272%3A_____%2F10%3A%230001282" target="_blank" >RIV/00023272:_____/10:#0001282 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

The supergene mineral association with brandholzite from Pernek, Malé Karpaty Mountains, Slovak Republic

Popis výsledku v původním jazyce

Brandholzite, a hydrated hydroxide of Mg2+ and Sb5+, was found at the Krížnica deposit near Pernek (Malé Karpaty Mountains, Slovak Republic); it is the second occurrence of this mineral phase worldwide. Crystals and crusts of brandholzite occur as surface coatings on altered rocks mineralized with stibnite and pyrite. Associated minerals include roméite-like phases, sulphur, aragonite, gypsum, sénarmontite and Sb-rich Fe-hydroxides. Brandholzite forms euhedral tabular crystals of hexagonal habit, typically 0.5 to 0.8 mm across, exceptionally up to 2 mm long. All physical and chemical data are given in the paper. Brandholzite from Pernek and its mineral association were probably formed by sub-recent weathering processes in an abandoned mines environment.

Název v anglickém jazyce

The supergene mineral association with brandholzite from Pernek, Malé Karpaty Mountains, Slovak Republic

Popis výsledku anglicky

Brandholzite, a hydrated hydroxide of Mg2+ and Sb5+, was found at the Krížnica deposit near Pernek (Malé Karpaty Mountains, Slovak Republic); it is the second occurrence of this mineral phase worldwide. Crystals and crusts of brandholzite occur as surface coatings on altered rocks mineralized with stibnite and pyrite. Associated minerals include roméite-like phases, sulphur, aragonite, gypsum, sénarmontite and Sb-rich Fe-hydroxides. Brandholzite forms euhedral tabular crystals of hexagonal habit, typically 0.5 to 0.8 mm across, exceptionally up to 2 mm long. All physical and chemical data are given in the paper. Brandholzite from Pernek and its mineral association were probably formed by sub-recent weathering processes in an abandoned mines environment.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

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Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2010

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Journal of Geosciences

ISSN

1802-6222

e-ISSN

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Svazek periodika

55

Číslo periodika v rámci svazku

2

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

12

Strana od-do

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Kód UT WoS článku

000286341800005

EID výsledku v databázi Scopus

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