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Copper-bearing Glauconite

A variety of 'Glauconite'
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Formula:
(K,Na)(Mg,Fe2+,Fe3+,Cu)(Fe3+,Al)(Si,Al)4O10(OH)2
Crystal System:
Monoclinic
A 2M polytype mica, glauconite variety, containing up to 2.02 wt.% CuO and anomalously rich in Na2O (over 6 wt.%) and MgO (over 7 wt.%), by up to 1.13 wt.% FeO.

A common constituent of white sandstones (Weissliegendes) with chalcocite mineralization within the Zechstein Cu deposits of Fore-Sudetic Monocline, Poland. Likely a product of an interaction of ordinary glauconite with Mg,K-bearing brine being at once parental to the Cu mineralization.


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Unique IdentifiersHide

Mindat ID:
47544 (as Copper-bearing Glauconite)
1710 (as Glauconite)
Long-form identifier:
mindat:1:1:47544:0 (as Copper-bearing Glauconite)
mindat:1:1:1710:3 (as Glauconite)

Chemistry of Copper-bearing GlauconiteHide

Mindat Formula:
(K,Na)(Mg,Fe2+,Fe3+,Cu)(Fe3+,Al)(Si,Al)4O10(OH)2
Element Weights:
Element% weight
O45.111 %
Si26.396 %
Fe13.122 %
K9.187 %
Mg5.711 %
H0.474 %

Calculated from ideal end-member formula.

Crystallography of Copper-bearing GlauconiteHide

Crystal System:
Monoclinic
Cell Parameters:
a = 5.19 Å, b = 9.00 Å, c = 19.99 Å
β = 95.48°
Ratio:
a:b:c = 0.577 : 1 : 2.221
Unit Cell V:
929.47 ų (Calculated from Unit Cell)

Synonyms of Copper-bearing GlauconiteHide

RadioactivityHide

Other InformationHide

Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.

Internet Links for Copper-bearing GlauconiteHide

References for Copper-bearing GlauconiteHide

Localities for Copper-bearing GlauconiteHide

ⓘ - Click for references and further information on this occurrence. ? - Indicates mineral may be doubtful at this locality. - Good crystals or important locality for species. - World class for species or very significant. (TL) - Type Locality for a valid mineral species. (FRL) - First Recorded Locality for everything else (eg varieties). Struck out - Mineral was erroneously reported from this locality. Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).

All localities listed without proper references should be considered as questionable.
Poland
 
  • Lower Silesian Voivodeship
Kucha et al. (1982)
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