| Element | % | | Oxide | % |
| O | 44.30 | | | |
| Mg | 11.66 | | MgO | 19.33 |
| Al | 11.28 | | Al2O3 | 21.32 |
| Si | 19.38 | | SiO2 | 41.45 |
| Ca | 3.32 | | CaO | 4.65 |
| Ti | 0.70 | | TiO2 | 1.16 |
| Cr | 0.39 | | Cr2O3 | 0.58 |
| Mn | 0.21 | | MnO | 0.27 |
| Fe | 8.67 | | FeO | 11.15 |
|
|
|
| Sum | 99.9 | | Sum | 99.9 |
|
|  | |
| 200 µ m
| |
|
This is a reflected light micrograph of polished, carbon coated pyrope crystals.
The identifying etched label, which is a feature
of our standards, is invaluable for navigating in an electron beam instrument.
This pyrope is one of the so-
called "indicator minerals" prized when prospecting for diamonds.
In fact this Cr-poor garnet comes from suite of garnets from a
diamond mine in South Africa and is typical of a kimberlite
association. As can be seen, the crystals are robust, taking a
good polish. The name pyrope refers to its "fiery color" (Greek
pyro - fire) as can be seen in the mount.
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