Djurleite

TSNB108
Mineral
First oxidation zoneSecond oxidation zoneSulphide oresThird oxidation zoneHypogene (?)Supergene

Mineral Species

Djurleite

Type Locality

No

Composition

Cu31S16

Crystal System

Monoclinic

Status at Tsumeb

Confirmed

Abundance

Very common

Distribution

First, second and third oxidation zones; sulphide ores

Paragenesis

Hypogene (?); supergene

Entry Number

Species; TSNB108

General Notes

Djurleite was described as a new mineral by Roseboom (1962) following studies of synthetic copper sulphides by Djurle (1958), after whom the mineral is named. Roseboom (1962) recognised one of Djurle’s compounds in natural ores from a number of localities including Tsumeb, although his paper does not provide a specific type locality.


Hughes (1987) listed djurleite as a major component of sulphide ores at Tsumeb and suggested that most of it is probably of supergene origin.


According to Gebhard (1999) excellent crystals of "chalcocite" found in the third oxidation zone, between 44 and 47 levels, are in fact a 50:50 mixture of chalcocite and djurleite.




Associated Minerals

betpakdalite-CaMg; bornite; calvertite; chalcocite; digenite; galena; scorodite