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Troilite () is a rare iron sulfide mineral with the simple formula of FeS. It is the iron-rich endmember of the pyrrhotite group. Pyrrhotite has the formula Fe(1−x)S (x = 0 to 0.2) which is iron deficient. As troilite lacks the iron deficiency which gives pyrrhotite its characteristic magnetism, troilite is non-magnetic.

Key facts

Mineral.name
Troilite
Mineral.image
Mundrabilla.jpg
Mineral.imagesize
260px
Mineral.caption
Polished and etched surface of the Mundrabilla meteorite from Australia. The darker brownish areas with striations are troilite with exolved daubréelite.
Mineral.category
Sulfide mineral
Mineral.formula
FeS
Mineral.IMAsymbol
Tro
Mineral.strunz
2.CC.10
Mineral.system
Hexagonal
Mineral.class
Ditrigonal dipyramidal (m2) H-M symbol: (m2)
Mineral.symmetry
P2c
Mineral.unit cell
a = 5.958, c = 11.74 [Å]; Z = 12
Mineral.color
Pale gray brown
Mineral.habit
Massive, granular; nodular; platey to tabular
Mineral.cleavage
None
Mineral.fracture
Irregular
Mineral.mohs
3.5–4.0
Mineral.luster
Metallic

via Wikipedia infobox

Wikidata facts

Image
Sikhote alin.jpg
Show 6 more facts
IMA Mineral Symbol
Tro
Commons category
Troilite
Nickel-Strunz 9th edition (updated 2009)
2.CC.10
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
2.CC.10
chemical formula
FeS
Strunz 8th edition (series ID, updated)
II/B.09a
Sources (2)

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Article

5 sections
Contents
  • Structure
  • Discovery
  • Occurrence
  • See also
  • References

Troilite () is a rare iron sulfide mineral with the simple formula of FeS. It is the iron-rich endmember of the pyrrhotite group. Pyrrhotite has the formula Fe(1−x)S (x = 0 to 0.2) which is iron deficient. As troilite lacks the iron deficiency which gives pyrrhotite its characteristic magnetism, troilite is non-magnetic.

Troilite can be found as a native mineral on Earth but is more abundant in meteorites, in particular, those originating from the Moon and Mars. It is among the minerals found in samples of the meteorite that struck Russia in Chelyabinsk on February 15th, 2013. Uniform presence of troilite on the Moon and possibly on Mars has been confirmed by the Apollo, Viking and Phobos space probes. The relative intensities of isotopes of sulfur are rather constant in meteorites as compared to the Earth minerals, and therefore troilite from Canyon Diablo meteorite is chosen as the international sulfur isotope ratio standard, the Canyon Diablo Troilite (CDT).

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