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Minnesotaite
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Minnesotaite
Minnesotaite
General
CategoryPhyllosilicate minerals, pyrophyllite-talc group
Formula(Fe2+,Mg)3Si4O10(OH)2
IMA symbolMns[1]
Strunz classification9.EC.05
Crystal systemTriclinic
Crystal classPinacoidal (1)
(same H-M symbol)
Space groupP1
Unit cella = 5.623(2) Å,
b = 9.419(2) Å,
c = 9.624(3) Å;
α = 85.21(3)°, β = 95.64(3)°,
γ = 90.00°; Z = 2
Identification
ColorGreenish gray to olive-green
Crystal habitOccurs as microscopic needles or platelets, the needles occur in radiating clusters or in sheaves; also fibrous
TwinningInferred based on X-ray patterns
CleavagePerfect on {001}, micaceous
FractureUneven and irregular
TenacityBrittle
Mohs scale hardness1.5 - 2
LusterGreasy to waxy, dull
DiaphaneityTranslucent
Specific gravity3.01
Optical propertiesBiaxial (-)
Refractive indexnα = 1.578 - 1.583 nβ = 1.578 - 1.622 nγ = 1.615 - 1.623
Birefringenceδ = 0.037 - 0.040
PleochroismX= pale green, Z= colorless to pale greenish yellow
2V angleMeasured: 4°
Dispersionr < v moderate
References[2][3][4]

Minnesotaite is an iron silicate mineral with formula: (Fe2+,Mg)3Si4O10(OH)2. It crystallizes in the triclinic crystal system and occurs as fine needles and platelets with other silicates.[2] It is isostructural with the pyrophyllite-talc mineral group.[3]

Occurrence

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Minnesotaite was first described in 1944 for occurrences in the banded iron formations of northern Minnesota for which it was named. Co-type localities are in the Cuyuna North Range, Crow Wing County and the Mesabi Range in St. Louis County.[3][5]

It occurs associated with quartz, siderite, stilpnomelane, greenalite and magnetite.[2][6] In addition to the low grade metamorphic banded iron formations it has also been reported as an alteration mineral associated with sulfide bearing veins.[3]

References

[edit]
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