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Carrollite information


Carrollite
Carrollite from Kambove, Katanga. This specimen is 4.3 cm wide, with a 1.2 cm carrollite crystal partly covered by pyrite, between calcite crystals.
General
CategorySulfide mineral
Thiospinel group (Spinel structural group)
Formula
(repeating unit)
CuCo2S4
IMA symbolCli[1]
Strunz classification2.DA.05
Dana classification2.10.1.2
Crystal systemIsometric
Crystal classHexoctahedral (m3m)
H-M symbol: (4/m 3 2/m)
Space groupFd3m
Identification
ColorLight to dark gray, rarely tarnishes to copper red or violet gray
Crystal habitOctahedral and cubic crystals, also massive, granular or compact
Twinning{111} Polysynthetic or spinel twins[2]
CleavageImperfect on {001}
FractureConchoidal, subconchoidal or uneven
TenacityVery brittle
Mohs scale hardness4.5 to 5.5
LusterMetallic
StreakGrey black
DiaphaneityOpaque. R is 43% to 45% for lambda = 560 nm[3]
Specific gravity4.5 to 4.8 measured, 4.83 calculated
Refractive indexn is not determined for an opaque mineral
SolubilityMinerals of the linneite group are partly etched by nitric acid, with slight effervescence.[2]
Other characteristicsNot radioactive, not fluorescent
References[4][5][6][7]

Carrollite, CuCo2S4, is a sulfide of copper and cobalt, often with substantial substitution of nickel for the metal ions, and a member of the linnaeite group. It is named after the type locality in Carroll County, Maryland, US, at the Patapsco mine, Sykesville.[6]

  1. ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
  2. ^ a b Ramdohr, R (1980) The Ore Minerals and their Intergrowths. Pergamom.
  3. ^ Criddle, A J and Stanley, C J (1993) Quantitative data file for ore minerals. Chapman & Hall page 74
  4. ^ Mineralienatlas
  5. ^ "Carrollite Mineral Data".
  6. ^ a b http://www.mindat.org/min-911.html Mindat.org
  7. ^ http://rruff.geo.arizona.edu/doclib/hom/carrollite.pdf Handbook of Mineralogy

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