Annite: Difference between revisions
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|molecular weight = 512.88 g |
|molecular weight = 512.88 g |
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|color = reddish brown |
|color = reddish brown |
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|habit = usually in "blocks" of thin sheets or as aggregations of foliated thin scales. Includes large, well formed pseudohexagonal prisms up to |
|habit = usually in "blocks" of thin sheets or as aggregations of foliated thin scales. Includes large, well formed pseudohexagonal prisms up to 12 cm across and 15 cm long.<ref>Hazen, R.M. and C.W. Burnham (1973) The crystal structures |
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of one-layer phlogopite and annite. Amer. Mineral., 58, 889{900.</ref> |
of one-layer phlogopite and annite. Amer. Mineral., 58, 889{900.</ref> |
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|system = monoclinic, pseudohexagonal |
|system = monoclinic, pseudohexagonal |
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|twinning = contact twins with composition surface on {001} and twin axis {310} |
|twinning = contact twins with composition surface on {001} and twin axis {310} |
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|cleavage = perfect in one direction {001}<ref> |
|cleavage = perfect in one direction {001}<ref>Deer, W.A., R.A. Howie, and J. Zussman (1963) Rock-forming minerals, v. 3, sheet silicates, |
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55{84}. |
55{84}.</ref> |
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|fracture = uneven |
|fracture = uneven |
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|tenacity = flexible<ref> |
|tenacity = flexible<ref>Eugster, H.P. and D.R. Wones (1962) Stability relations of the ferruginous biotite, |
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annite. J. Petrol., 3, 82{125.</ref> |
annite. J. Petrol., 3, 82{125.</ref> |
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|mohs = 2.5 - 3 |
|mohs = 2.5 - 3 |
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|luster = submetallic to vitreous; pearly on cleavage surfaces<ref> |
|luster = submetallic to vitreous; pearly on cleavage surfaces<ref>Dana, E.S. (1892) Dana's system of mineralogy, (6th edition), 634.</ref> |
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|optical properties = translucent to transparent<ref>Kwak, T.A.P. and P.W. |
|optical properties = translucent to transparent<ref>Kwak, T.A.P. and P.W. |
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Askins (1981) Geology and genesis of the F-Sn-W(-Be-Zn) skarn (wrigglite) at Moina, Tasmania. |
Askins (1981) Geology and genesis of the F-Sn-W(-Be-Zn) skarn (wrigglite) at Moina, Tasmania. |
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</references> |
</references> |
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==References== |
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{{Reflist}} |
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[[Category:Mica group]] |
[[Category:Mica group]] |
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{{Silicate-mineral-stub}} |
Revision as of 11:06, 29 September 2010
Annite is a phyllosilicate mineral in the mica family. It has a chemical formula of KFe32+[(OH)2]AlSi3O10]. [1] Annite is the iron end member of the biotite mica group, the iron rich analogue of magnesium rich phlogopite.[2]
Annite was first described in 1868 for the first noted occurrence in Cape Ann, Rockport, Essex County, Massachusetts, USA and on Pikes Peak, El Paso Co, Colorado.[1] It occurs in igneous and metamorphic rocks that are deficient in magnesium. It occurs associated with fluorite and zircon in the type locality.[3]
Annite | |
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General | |
Category | mica group, biotite-phlogopite series. The hydroxyll analogue of Flourannite. |
Formula (repeating unit) | KFe32+[(OH)2]AlSi3O10 |
Crystal system | monoclinic, pseudohexagonal |
Identification | |
Color | reddish brown |
Crystal habit | usually in "blocks" of thin sheets or as aggregations of foliated thin scales. Includes large, well formed pseudohexagonal prisms up to 12 cm across and 15 cm long.[4] |
Twinning | contact twins with composition surface on {001} and twin axis {310} |
Cleavage | perfect in one direction {001}[5] |
Fracture | uneven |
Tenacity | flexible[6] |
Mohs scale hardness | 2.5 - 3 |
Luster | submetallic to vitreous; pearly on cleavage surfaces[7] |
Streak | brownish white |
Specific gravity | approximately 3.3 g/cm3 |
Density | 3.17g |
Other characteristics | diagnostic: transparent to subopaque; occurrence: in magnesium poor igneous and metamorphic rocks. </references> |
References
- ^ a b Mindat.org
- ^ Deer, W. A., R. A. Howie and J. Zussman, An Introduction to the Rock Forming Minerals, Longman, 1966, p. 212 ISBN 0582442109
- ^ Handbook of Mineralogy
- ^ Hazen, R.M. and C.W. Burnham (1973) The crystal structures of one-layer phlogopite and annite. Amer. Mineral., 58, 889{900.
- ^ Deer, W.A., R.A. Howie, and J. Zussman (1963) Rock-forming minerals, v. 3, sheet silicates, 55{84}.
- ^ Eugster, H.P. and D.R. Wones (1962) Stability relations of the ferruginous biotite, annite. J. Petrol., 3, 82{125.
- ^ Dana, E.S. (1892) Dana's system of mineralogy, (6th edition), 634.
- ^ Kwak, T.A.P. and P.W. Askins (1981) Geology and genesis of the F-Sn-W(-Be-Zn) skarn (wrigglite) at Moina, Tasmania. Econ. Geol., 76, 439{467).
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