Pyrrhotite is an unusual
iron sulfide mineral with a variable iron content: Fe(1-x)S (x = 0 to 0.2). The FeS endmember is known as troilite. Also called magnetic
pyrite because the color is similar to pyrite and it is weakly magnetic, the
magnetism increases as the iron content decreases.Pyrrhotite is odd also because it has two crystal symmetries. When pyrrhotite is high in iron and the formula is closer to true FeS the structure is hexagonal. But, when it is low in iron, the structure is monoclinic. Both symmetries occur together in the same specimen.The name is derived from Greek pyrrhos, flame-colored.
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General Information:

Chemical Formula:
Fe(1-x)S (x=0-0.17)

Composition:
(Molecular Weight = 85.12 gm)
Iron 62.33 %
FeSulfur 37.67 %
S 
Empirical Formula:
Fe2+0.95S

Environment:
Wide spread occurrences in igneous and metamorphic rocks.

Locality:
Sudbury, Ontario, Canada and Santa Eulalia, Chihuahua, Mexico.

Name Origin:
From the Greek, phrrhotes, "redness," in allusion to color.
Physical Properties:

Cleavage:
[0001] Imperfect, [1120] Imperfect

Color:
bronze, bronze red, or dark brown.

Density:
4.58 - 4.65, Average = 4.61

Diaphaniety:
Opaque

Habits:
Tabular - Form dimensions are thin in one direction., Platy - Sheet forms (e.g. micas)., Massive - Granular - Common texture observed in granite and other igneous rock.

Hardness:
3.5-4 - Copper Penny-Flourite

Luminescence:
None.

Luster:
Metallic

Streak:
gray black
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