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The above photo is a hand specimen of dolomite with a greenish
variety of muscovite, known as fuchsite. The muscovite is high in
chromium where chromium replaces aluminium in the crystal structure. The photo above right is a thin section of the same rock scanned with crossed polars. It shows the very high birefringence of dolomite, almost white, as well as the typical rhombohedral twin lamellae seen towards the bottom right. The bright interference colours of fuchsite are visible on the left. For further information on fuchsite cf. cf. www.mindat.org/min-1617.html Top of page Back to thumbnails
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