During the long winter months in the Northland I enjoy
sorting through the many Perky Boxes that have accumulated during my mineral
wandering. The other day, as I was contemplating the fact we have gained 3
hours and 30 minutes of daylight since the December Winter Solstice, I pulled
out a specimen with several small notes stuffed in, or tapped to, the box. The
specimen was djurleite, a copper sulfide (Cu31S16), with
a confusing collecting history; hence, my stuffed notes from a past deciphering
episode.
Djurleite is a member of the Chalcocite Group, all members
being copper sulfides not known for their beauty. These sulfides are typically
black in color with a luster ranging from metallic to dull unless a light hits
them and they appear in various shades of gray. All are opaque, and quite soft
at about 2.5—3.0 (Mohs). One essentially needs an XRD to make a final
identification. A statement from Pósfai and Buseck (1964) seems way above my
paygrade: “chalcocite easily converts to djurleite under electron beam through
the rearrangement of Cu atoms.” That publication appeared at the time in my
undergraduate life when I was enrolled in a Mineralogy and suffering through
crystallography. Electron beams rearranging atoms was nowhere in my vocabulary.
Another fascinating item about djurleite is that that the mineral was named for
Dr. Seved Djurle, a professor of Chemistry at the University o Uppsala in
Sweden. Dr. Djurle was not a rockhound nor geologist but a chemist who
synthesized djurleite before the mineral was discovered. That tidbit seems
quite impressive to me!
So, back to the collecting history of my specimen. My purchase was made four years ago in Tucson from Michael Shannon and was an Ex David Shannon. The collecting locality on the ID card stated Djurleite, Reutanieme, Lapland, Sweden. A small cryptic note simply said “XRD.” So off to Mindat where Reutanieme was not listed as a collecting locality for any mineral nor was djurleite listed as a mineral found in Swedish Lapland. What’s an ole plugger like me to do? Well, for starters, hit the Internet! And guess what I found? From 2021 a question in the MinDat Discussion Group about Djurleite: “Collecting information for a specimen in the collection of minerals with Ingemar Johanson, including djurleite from the Naesmark site, Norway. See photo. I hope this will help you further.”
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Label of Djurleite in the collection of Andŕe Heyninck. From MinDat Discussion Group (accessed February 2025).
Therefore, off I went from Sweden hopping over to Norway and the Naesmark Mine. The Naesmark is part of a collection of copper mines generally assigned to the Amdals Verk Mine/District in Telemark. I cannot locate much information about the mines and mining activity except that MinDat (February 2025) lists 417 minerals known from Telemark and djurleite is rarely noted. This scarcity may be due to its relationship with chalcocite and digenite as perhaps all were mixed together and tossed into the processing plant. After all, who would want to collect pretty ugly black specimens?Above photomicrographs with width FOV ~6 mm. Some show very shiny metallic luster while others point to a dull metallic luster. All are associated with quartz.
So, what am I supposed to do about collecting locality
for my specimens? I could just leave it alone with the Reutaneeme, Lapland,
Sweden notation, or I could switch the locality to the Naesmark, Telemark,
Norway notation. Since my specimen looks “very related” to my specimen photo on
MinDat I will go with the Norway collecting site. However, it could be from
Sweden (doubtful) or one of several mines in Norway (likely).
That is about my total knowledge of the copper sulfide
djurleite. It seems somewhat uncommon in copper mining areas when one examines
total “numbers” of specimens. However, my uneducated thought is that djurleite
is often mistaken for common chacosite.in the enriched supergene copper
deposits.
REFERENCES
CITED
Pósfai, M. and
Buseck, P. R., 1994, Djurleite, digenite, and chalcocite: Intergrowths and
transformations: American Mineralogist, No. 79.