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| Molybdenite
is named from the Greek molybdos
for lead.
| Discovered
in 1807.
IMA
status: Valid (pre-IMA; Grandfathered) |
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Chemistry
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Chemical
Formula: |
MoS2 |
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Molybdenum
Sulfide |
Molecular
Weight: |
160.07 gm |
Composition: |
Molybdenum |
59.94 %
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Mo
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Sulfur |
40.06 %
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S
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100.00 % |
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Classification
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Mineral
Classification: |
Sulfides
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Strunz 8th
Ed. ID:
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2/D.25-10
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Nickel-Strunz 10th
Ed. ID:
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2.EA.30
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2 : SULFIDES and SULFOSALTS (sulfides, selenides,
tellurides; arsenides, antimonides, bismuthides; sulfarsenites,
sulfantimonites, sulfbismuthites, etc.) E : Metal Sulfides, M: S <= 1:2 A : M:S = 1:2 - With Cu, Ag, Au
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Related
to: |
Molybdenum
Group. Dimorphous with Jordisite. Two polytypes are known: Molybdenite-2H
(very common) and Molybdenite-3R (rare).
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Varieties: |
Femolite,
Rhenian Molybdenite
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Synonyms: |
Castaingite-(Cu),
Molybdic Ochre, Muchuanite - a mixture of Molybdenite
and Jordisite
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Crystal
Data
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Crystallography:
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Hexagonal
- Dihexagonal Dipyramidal
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Crystal
Habit:
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Crystals
are commonly tabular, barrel shaped; also as slightly
tapered prisms; face development poor; up to 15 cm across.
Commonly shows trigonal markings on {0001} parallel
to the trace of {1011}. Foliated, massive, or in scales.
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Twinning:
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None
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Physical
Properties
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Cleavage: |
[0001]
Perfect
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Fracture: |
Sectile
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Tenacity:
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Lamellae
flexible, not elastic
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Moh's
Hardness: |
1.0
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Density:
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4.62
- 4.73 (g/cm3)
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Luminescence:
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None |
Radioactivity:
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Not
Radioactive
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Optical
Properties
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Color: |
Black,
lead Gray, Gray, Silvery Black with a Bluish cast
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Transparency: |
Opaque
to nearly
Opaque; translucent in thin flakes; transparent in infrared
light
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Luster: |
Metallic
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Refractive
Index: |
R1–R2:
(400) 21.0–55.0, (420) 22.2–54.8, (440) 23.4–54.6, (460)
24.1–53.8, (480) 23.8–52.3, (500) 22.7–49.7, (520) 21.9–47.1,
(540) 21.3–45.5, (560) 20.9–44.4, (580) 20.6–44.0, (600)
20.4–44.6, (620) 20.2–45.3, (640) 20.0–45.7, (660) 20.0–45.6,
(680) 19.9–45.4, (700) 19.7–44.2
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Birefringence: |
0.0140
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Pleochroism: |
Very
Strong
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Anisotrophism: |
Very
Strong; Color in reflected light: gray, very pale yellow to deep reddish brown in transmitted light.
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Occurances
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Geological
Setting: |
In
high-temperature hydrothermal veins. In disseminated
deposits of the porphyry type, both with and without
associated major copper mineralization. Also in contact
metamorphic deposits in limestone with calcium silicate
minerals as well as in pegmatites, granites, and aplites.
Rarely in meteorites. |
Common
Associations: |
Chalcopyrite,
other copper sulfides |
Type
Locality: |
Common world wide occurrences |
Year
Discovered: |
1807 |
View
mineral photos: |
Molybdenite
Mineral Photos and Locations |
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More
Information
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Mindat.org Webmineral.com
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Molybdenite
is a very soft metallic mineral that is rarely available
as a faceted gem. Due to its color and softness, it
can easily be confused with Graphite. Graphite is a
slightly darker silvery black and Molybdenite is usually
silvery black with a bluish cast. Molybdenite however
has a greater density of 4.62 - 4.73 than Graphite's
2.09 - 2.23. Both are soft enough to leave black on
your fingers when handling. Molybdenite is slight softer
at 1.0 on the Moh's scale, while Graphite is about 1.0
- 2.0. Because of its extreme softness and metallic
luster, Molybdenite has a greasy feel.
Molybdenite
is of widespread occurrence; the most abundant molybdenum
mineral. Fine crystals occur, in the USA, at the Crown
Point mine, Lake Chelan, Chelan County, Washington;
and at the Frankford quarry, Philadelphia, Pennsylvania.
In Canada, in the Temiskaming district, and in Aldfield
Township, Quebec. In Norway, from Raade, near Moss,
and at Vennesla, near Arendal. In Russia, in the Adun-Chilon
Mountains, south of Nerchinsk, Transbaikal; at Miass,
Ilmen Mountains, Southern Ural Mountains; and in the
Slundyanogorsk deposit, Central Ural Mountains. In Germany,
at Altenberg, Saxony. In Morocco, at Azegour, 80 km
southwest of Marrakesh. From Kingsgate and Deepwater,
New South Wales, Australia. At the Hirase mine, Gifu
Prefecture, Japan. In the Wolak mine, Danyang, Chungchong
Province, South Korea. The 3R polytype occurs in the
Con mine, Yellowknife, Yukon Territory; and at Mont
Saint-Hilaire, Quebec, Canada. From the Yamate mine,
Okayama Prefecture, Japan.
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