![](../images/Fluorescence/Mn_Minerals_Fluorescence_Transmission_I.jpg) |
Figure 1: transmission fluorescence
image of a section of mangano-calcite and forsterite from Sweden. The
mangano-calcite is fluorescent.
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![](../images/Fluorescence/Mn_Minerals_Reflex_LPNA_I.jpg) |
Figure 2: same section in plane
polarized light. The dark mineral is hausmanite.
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![](../images/Fluorescence/Mn_minerals_fluorescence_reflexion_composite_I.jpg) |
Figure 3: same mangano-calcite
sample fluorescence in reflection.
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![](../images/Fluorescence/Mn_minerals_R_LPNA_I.jpg) |
Figure 4: transmission plane
polarized view.
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![](../images/Fluorescence/Mn_minerals_R_LPA_I.jpg) |
Figure 5: crossed polars view. The
bright interference colors come from forsterite.
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![](../images/Fluorescence/Zn-Minerals_Fluorescence_LRGB_I.jpg) |
Figure 6: another sample from the
same place. Transmission fluorescence.
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![](../images/Fluorescence/Zn_minerals_fluorescence_reflection_I.jpg) |
Figure 7: same sample viewed in
reflection fluorescence. The fluorescence seems to originate from the
rims of the crystals.
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![](../images/Fluorescence/zn_minerals_LPNA_I.jpg) |
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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![](../images/Fluorescence/Spectra_Manganocalcite.png) |
Figure 9: fluorescence spectra of
the two samples recorded with the Alpy 600.
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