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		| Figure 1: transmission fluorescence 
		image of a section of mangano-calcite and forsterite from Sweden. The 
		mangano-calcite is fluorescent.   | 
	
		|  | 
	
		| Figure 2: same section in plane 
		polarized light. The dark mineral is hausmanite.   | 
	
		|  | 
	
		| Figure 3: same mangano-calcite 
		sample fluorescence in reflection.   | 
	
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		| Figure 4: transmission plane 
		polarized view.   | 
	
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		| Figure 5: crossed polars view. The 
		bright interference colors come from forsterite.   | 
	
		|  | 
	
		| Figure 6: another sample from the 
		same place. Transmission fluorescence.   | 
	
		|  | 
	
		| Figure 7: same sample viewed in 
		reflection fluorescence. The fluorescence seems to originate from the 
		rims of the crystals.   | 
	
		|  | 
	
		| Figure 8: same section in 
		transmission plane polarized view. A higher amount of opaque hausmanite  and less 
		forsterite can be seen compared to the first sample.   | 
	
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		| Figure 9: fluorescence spectra of 
		the two samples recorded with the Alpy 600.   |