Mineral species in the context of "Mineral group"

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⭐ Core Definition: Mineral species

In geology and mineralogy, a mineral or mineral species is, broadly speaking, a solid substance with a fairly well-defined chemical composition and a specific crystal structure that occurs naturally in pure form.

The geological definition of mineral normally excludes compounds that occur only in living organisms. However, some minerals are often biogenic (such as calcite) or organic compounds in the sense of chemistry (such as mellite). Moreover, living organisms often synthesize inorganic minerals (such as hydroxylapatite) that also occur in rocks.

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πŸ‘‰ Mineral species in the context of Mineral group

In geology and mineralogy, a mineral group is a set of mineral species with essentially the same crystal structure and composed of chemically similar elements.

For example, the amphibole group consists of 15 or more mineral species, most of them with the general unit formula A
x
B
y
C
14-3x-2y
Si
8
O
22
(OH)
2
, where A is a trivalent cation such as Fe
or Al
, B is a divalent cation such as Fe
, Ca
, or Mg
, and C is an alkali metal cation such as Li
, Na
, or K
. In all these minerals, the anions consist mainly of groups of four SiO
4
tetrahedra connected by shared oxygen corners so as to form a double chain of fused six-member rings. In some of the species, aluminum Al
may replace some silicon atoms Si
in the backbone, with extra B or C cations to balance the charges.

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Mineral species in the context of Azure spar

Azure spar, sometimes azur-spar, is a trivial and commercial, partly obsolete name for several of the most famous bright blue or blue-colored minerals, which also have similar names, most notably for lazurite and azurite, and also for the less commonly used lazulite.

In addition, Robert Jameson in his fundamental works of 1804-1821 also included hauyne as a separate mineral species and the so-called β€œcalaite”, which in the 1820s meant only turquoise, among the azure feldspars.

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