Ankerite: Difference between revisions
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Revision as of 11:57, 14 October 2016
Ankerite | |
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General | |
Category | Carbonate mineral |
Formula (repeating unit) | Ca(Fe,Mg,Mn)(CO3)2 |
Strunz classification | 5.AB.10 |
Crystal system | Trigonal Rhombohedral class |
Space group | Trigonal H-M symbol: (3) Space group: R3 |
Unit cell | a = 4.8312(2) c = 16.1663(3) [Å]; Z = 3 |
Identification | |
Color | Brown, yellow, white |
Crystal habit | Chrystals rhombohedral with curved faces; columnar, stalactitic, granular, massive |
Twinning | Simple twins on {0001}, {1010}. {1120} |
Cleavage | Perfect on {1011} |
Fracture | Subconchoidal |
Tenacity | Brittle |
Mohs scale hardness | 3.5–4 |
Luster | Vitreous to pearly |
Streak | White |
Diaphaneity | Translucent to transparent |
Specific gravity | 2.93–3.10 |
Optical properties | Uniaxial (-) |
Refractive index | nω = 1.690 - 1.750 nε = 1.510 - 1.548 |
Birefringence | δ = 0.180 - 0.202 |
Dispersion | Strong |
References | [1][2][3] |
Ankerite is a calcium, iron, magnesium, manganese carbonate mineral of the group of rhombohedral carbonates with formula: Ca(Fe,Mg,Mn)(CO3)2. In composition it is closely related to dolomite, but differs from this in having magnesium replaced by varying amounts of iron(II) and manganese. Forms series with dolomite and kutnohorite.[2]
![](http://upload.wikimedia.org/wikipedia/commons/thumb/5/52/Ankerite%2C_Pyrite_-_Goldmyer_Hot_Springs%2C_King_Co%2C_Washington%2C_USA.jpg/220px-Ankerite%2C_Pyrite_-_Goldmyer_Hot_Springs%2C_King_Co%2C_Washington%2C_USA.jpg)
The crystallographic and physical characters resemble those of dolomite and siderite. The angle between the perfect rhombohedral cleavages is 73° 48', the hardness is 3.5 to 4, and the specific gravity is 2.9 to 3.1. The color is white, grey or reddish to yellowish brown.
Ankerite occurs with siderite in metamorphosed ironstones and sedimentary banded iron formations. It also occurs in carbonatites. In sediments it occurs as authigenic, diagenetic minerals and as a product of hydrothermal deposition.[1] It is one of the minerals of the dolomite-siderite series, to which the terms brown-spar, pearl-spar and bitter-spar have been historically loosely applied.
It was first recognized as a distinct species by W. von Haidinger in 1825, and named for Matthias Joseph Anker (1771–1843) of Styria, an Austrian mineralogist.[2]
See also
References
public domain: Chisholm, Hugh, ed. (1911). "Ankerite". Encyclopædia Britannica (11th ed.). Cambridge University Press.
This article incorporates text from a publication now in theExternal links
![](http://upload.wikimedia.org/wikipedia/en/thumb/4/4a/Commons-logo.svg/30px-Commons-logo.svg.png)