Английская Википедия:Ankerite

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Шаблон:Short description Шаблон:Infobox mineral

Ankerite is a calcium, iron, magnesium, manganese carbonate mineral of the group of rhombohedral carbonates with the chemical formula Шаблон:Chem2. In composition it is closely related to dolomite, but differs from this in having magnesium replaced by varying amounts of iron(II) and manganese. It forms a series with dolomite and kutnohorite.[1]

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.[2]

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.[3] 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.[2]

It was first recognized as a distinct species by Wilhelm von Haidinger in 1825, and named for Matthias Joseph Anker (1771–1843) of Styria, an Austrian mineralogist.[1]

It has been found in Western Tasmania, in mines in Dundas, Tasmania.

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See also

References

Шаблон:Refbegin Шаблон:Reflist

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External links

Шаблон:Commons category

Шаблон:Manganese minerals

  1. 1,0 1,1 Ошибка цитирования Неверный тег <ref>; для сносок Mindat не указан текст
  2. 2,0 2,1 Шаблон:EB1911
  3. Ошибка цитирования Неверный тег <ref>; для сносок HBM не указан текст