| Element | % | | Oxide | % |
| H | 0.22 | | H2O | 1.97 |
| O | 42.83 | | | |
| Na | 1.81 | | Na2O | 2.44 |
| Mg | 7.57 | | MgO | 12.55 |
| Al | 6.54 | | Al2O3 | 12.36 |
| Si | 18.74 | | SiO2 | 40.09 |
| K | 0.97 | | K2O | 1.17 |
| Ca | 8.26 | | CaO | 11.56 |
| Ti | 3.02 | | TiO2 | 5.04 |
| Mn | 0.14 | | MnO | 0.18 |
| Fe | 9.51 | | FeO | 12.23 |
|
|
|
| Sum | 99.6 | | Sum | 99.6 |
|
|  | |
| 200 µ m
| |
|
This is a reflected light micrograph of polished, carbon coated
kaersutite crystals.
The identifying etched label, which is a feature
of our standards, is invaluable for navigating in an electron beam instrument.
Kaersutite is an
amphibole, which allows a wide range of chemical elements to enter
its structure. It therefore has many possibilities as a standard.
The moderate amounts of potassium, titanium and sodium, for
instance, as well as the more abundant silicon, aluminium and
calcium. It is named after the type locality, Kaersut, in Greenland.
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