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Formula: CuO
Simple oxide
Crystal System: Monoclinic
Specific gravity: 6.45 measured, 6.515 calculated
Hardness: 3½
Streak: Black
Colour: Grey-black
Environments:
Volcanic sublimates
Hydrothermal environments
Tenorite is a secondary copper
mineral present to some degree in virtually all
oxidised copper deposits. It is also a volcanic sublimate. Associated minerals include
cuprite, copper,
chrysocolla, malachite,
azurite and cotunnite (volcanic sublimates)
(HOM).
Localities
At the Girilambone mine, New South Wales, Australia, tenorite occurs in veins cutting
chlorite schist, associated with
malachite.
Elsewhere at the mine cuprite enclosed by tenorite is associated with
malachite and azurite in
quartz-hematite
gossan
(AJM 11.2.98).
At Johanngeorgenstadt, Erzgebirgskreis, Saxony, Germany, tenorite was found at the Getreue Einigkeit mine in the
Jugel Forest, where several tin ore veins associated with
copper minerals were exploited. In cavities, tenorite was found as
coatings on chalcopyrite, and as pure masses
(MinRec 55.5.621).
At Bisbee, Arizona, USA, tenorite is commonly associated with copper nodules
(MinRec 43.1 supplement).
Tenorite from Bisbee - Image
The Central Mine, Central, Keweenaw county, Michigan, USA, initially targeted a series of sub-parallel mineralised
fissure veins where the most copper-rich portion of the vein was close to the
base of the main greenstone flow.
Tenorite is common at the Central mine as black oxide coatings on some native
copper specimens, which impart a beautiful, often lustrous jet-black patina to
the copper crystals
(MinRec 54.1.81).
At the Copper Falls Mine, Copper Falls, Keweenaw county, Michigan, USA, mineralisation occurs primarily in hydrothermal veins
cutting preexisting lavas and as amygdules in the Ashbed flow.
Tenorite is common at the Copper Falls mine as black oxide coatings on some native
copper specimens, sometimes imparting a wonderful lustrous black patina on the
crystallised copper
(MinRec 54.1.113).
Alteration
In the oxidized zone chalcopyrite may be oxidised to yield Cu2+, and this
may cause the precipitation of copper oxides such
as tenorite:
Cu2+ + H2O → CuO (tenorite) + 2H+
The diagram below is a Pourbaix diagram for Cu-Fe-S-H2O
(IJNM 07(02).9.23).
It shows the relationship between copper Cu,
chalcopyrite CuFeS2,
tenorite CuO,
covellite CuS,
cuprite Cu2O,
chalcocite Cu2S,
pyrite FeS2 and
hematite Fe2O3.
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