(mineralogy) (Fe,Mg)7Si8O22(OH)2 A brownish mineral that crystallizes in the monoclinic system; usually occurs as lamellae or fibers in metamorphic rocks.
Cummingtonite
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(′kəm·iŋ·tə′nīt)
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An amphibole (a double-chain silicate mineral) with the idealized chemical formula Mg7Si8O22(OH)2 that crystallizes with monoclinic symmetry. Naturally occurring samples generally are solid solutions between Mg7Si8O22(OH)2 and the corresponding iron (Fe)-end member with the general formula (Mg,Fe)7Si8O22(OH)2. The name cummingtonite (derived from the location Cummington, Massachusetts) is applied to all solid solutions with Mg/(Mg + Fe2+) ≥ 0.5, whereas those with Mg/(Mg + Fe2+) < 0.5 are termed grunerite. Up to a total of 1.0 (Ca + Na) atom per formula unit may also be present in cummingtonite.
Cummingtonite commonly occurs as aggregates of fibrous crystals, often in radiating clusters. It is transparent to translucent, varies in color from white to green to brown, and may be pale to dark depending primarily on the iron content. Hardness is 5–6 on Mohs scale; density is 3.1–3.6 g/cm3 (1.8–2.1 oz/in.3), increasing with increasing iron content.
Cummingtonite is generally considered to be a metamorphic mineral, but it has been found in silicic volcanic rocks and, rarely, plutonic igneous rocks. It occurs in a variety of metamorphic rock types (amphibolite, schist, gneiss, granulite) that have undergone medium- to high-grade metamorphism. It commonly occurs in the calcium- and aluminum-poor environment of metamorphosed iron formation. It can also be a constituent of metamorphosed mafic and ultramafic igneous rocks, where it may coexist with other amphibole minerals such as hornblende, tremolite, and anthophyllite. With increasing intensity of metamorphism, cummingtonite is commonly replaced by pyroxene-bearing mineral assemblages. See also
| Wikipedia: Cummingtonite |
| Cummingtonite | |
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| General | |
| Category | Mineral |
| Chemical formula | (Mg,Fe)7Si8O22(OH)2 |
| Identification | |
| Color | Dark green - brown |
| Crystal habit | Rarely as distinct crystals. Columnar to fibrous and granular |
| Crystal system | Monoclinic; 2/m |
| Twinning | Simple and lamellar - common |
| Cleavage | 56 and 124° - good; {110} perfect |
| Fracture | Splintery |
| Mohs scale hardness | 5 - 6 |
| Luster | Vitreous - Silky |
| Diaphaneity | Translucent, will transmit light on thin edges. |
| Specific gravity | 3.1 - 3.6 |
| Optical properties | Optically (+) |
| Refractive index | nα=1.65 - 1.69, nβ=1.67 - 1.671, nγ=1.69 - 1.73 |
| Pleochroism | Non-pleochroic |
| Diagnostic features | Characterized by light brown color and needlelike, often radiating habit. difficult to distinguish from anthophyllite or gedrite without optical and/or X-ray tests. |
| References | [1][2][3] |
Cummingtonite is a metamorphic amphibole with the chemical composition (Mg,Fe)7Si8O22(OH)2, magnesium iron silicate hydroxide.
Monoclinic cummingtonite is compositionally similar and polymorphic with orthorhombic anthophyllite, which is a much more common form of magnesium-rich amphibole, the latter being metastable.
Cummingtonite shares few compositional similarities with alkali amphiboles such as arfvedsonite, glaucophane-riebeckite. There is little solubility between these minerals due to different crystal habit and inability of substitution between alkali elements and ferro-magnesian elements within the amphibole structure.
Cummingtonite was first described in 1824 for an occurrence near Cummington, Massachusetts, hence the name.[1][2] It is also found in Sweden, South Africa, and Scotland.
Chemistry
Cummingtonite is a member of the cummingtonite-grunerite solid solution series which ranges from Fe2Mg5Si8O22(OH)2 for cummingtonite to the iron rich grunerite endmember Fe7Si8O22(OH)2. Cummingtonite is used to describe minerals of this formula with between 30 and 70 per cent Fe7Si8O22(OH)2.
Manganese also substitutes for (Fe,Mg) within cummingtonite amphibole, replacing B site atoms. These minerals are found in high-grade metamorphic banded iron formation and form a compositional series between Mn2Mg5Si8O22(OH)2 (tirodite) and Mn2Fe5Si8O22(OH)2 (dannemorite).
Calcium, sodium and potassium concentrations in cummingtonite are low. Cummingtonite tends toward more Ca substitution than related anthophyllite. Similarly, cummingtonite has lower Fe3+ and Al than anthophyllite.
Amosite is a rare asbestiform variety of grunerite that is mined as asbestos only in the eastern part of the Transvaal Province of South Africa. The origin of the name is Amosa, the acronym for the mining company "Asbestos Mines of South Africa."
Occurrence
Cummingtonite is commonly found in metamorphosed magnesium-rich rocks and occurs in amphibolites. Usually it coexists with hornblende or actinolite, magnesium clinochlore chlorite, talc, serpentine-antigorite minerals or metamorphic pyroxene. Magnesium-rich cummingtonite can also coexist with anthophyllite.
Cummingtonite has also been found in some felsic igneous rocks such as dacites. Manganese rich species can be found in metamorphosed Mn-rich rock units. The grunerite end member is characteristic of the metamorphosed iron formations of the Lake Superior region and the Labrador Trough. With prograde metamorphism cummingtonite and grunerite morph to members of the olivine and pyroxene series.
References
- ^ a b http://rruff.geo.arizona.edu/doclib/hom/cummingtonite.pdf Handbook of Mineralogy, 2001, Mineral Data Pub.
- ^ a b http://www.mindat.org/min-1170.html Mindat data
- ^ http://webmineral.com/data/Cummingtonite.shtml Webmineral data
- Deer W.A., Howie R.A., & Zussman J. An Introduction to the Rock Forming Minerals, 2nd Edition, 1997, pp. 229-247.
- Hurlbut, Cornelius S.; Klein, Cornelis, 1985, Manual of Mineralogy, 20th ed., Wiley, ISBN 0-471-80580-7
- Klein, Cornelius., 2002, The Manual of Mineral Science, 22nd ed., John Wiley & Sons, Inc. ISBN 0-471-25177-1
- Mineral Galleries
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