Annite

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Annite
2V angle
Calculated: 12° to 36°
Other characteristicsDiagnostic: occurrence: in magnesium poor igneous and metamorphic rocks.
References[7][8]

Annite is a

phyllosilicate mineral in the mica family. It has a chemical formula of KFe32+AlSi3O10(OH)2.[8] Annite is the iron end member of the biotite mica group, the iron rich analogue of magnesium rich phlogopite.[9] Annite is monoclinic and contains tabular crystals and cleavage fragments with pseudohexagonal outlines.[6] There are contact twins with composition surface {001} and twin axis {310}.[10]

Annite was first described in 1868 for the first noted occurrence in

metamorphic rocks that are deficient in magnesium and is associated with fluorite and zircon in the type locality.[8]

Properties

The relief of a mineral refers to the way a mineral may stand out in plane polarized light. A mineral may be referred to as having a low or high relief. Minerals with a high relief, such as annite, have sharp grain boundaries and display good fracture and cleavage. When viewed under a microscope, this mineral may appear to stick out of the other minerals in the thin section. Relief primarily depends on the index of refraction of the mineral.

pleochroic, meaning the mineral changes colors under a microscope without the polars being crossed.[8]

Uses

Annite is a member of the mica group and has very similar properties as other micas such as muscovite and biotite. More importantly, annite is interesting to geologists because it can be used for potassium-argon dating. Because annite contains large amounts of potassium, it can be used to find the absolute age of articles older than 1000 years. This type of dating also preserves a record of the direction and intensity of the local magnetic field, giving field geologists better knowledge of their surroundings.[11]

References

  1. S2CID 235729616
    .
  2. ^ Hazen, R.M. and Burnham, C.W. (1973) The crystal structures of one-layer phlogopite and annite. American Mineralogist, 58, 889–900.
  3. ^ Deer, W.A., Howie, R.A., and Zussman, J. (1963) Sheet Silicates. Rock-forming minerals Volume 3, 55–84.
  4. ^ Eugster, H.P. and Wones, D.R. (1962) Annite. Stability relations of the ferruginous biotite. 3, 82–125
  5. ^ Dana, E.S. (1892) Dana's system of mineralogy, (6th edition), 634.
  6. ^ a b Kwak, T.A.P. and Askins, P.W. (1981) Geology and genesis of the F-Sn-W(-Be-Zn) skarn (wrigglite) at Moina, Tasmania. Economical Geology, 76, 439–467
  7. ^ a b c Mindat.org
  8. ^ a b c d e f Handbook of Mineralogy
  9. ^ Anthony,J.W., Bideaux, R.A., Bladh, K.W., and Nichols, C.M. (1995), Handbook of Mineralogy, Volume II, Silica, Silicates Part 1, p. 31
  10. ^ Eugster, H.P. and Wones, D.R.(1962) Stability relations of the ferruginous biotite, annite. 3, 82–125
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