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Importantly, the hyperspectral derived mineral map provided much greater detail enabling a more precise understanding of the regolith-geological architecture where there are exposed soils and rocks.
The calcified islands in Calc1 seen on the left of the mineral map in Figure 2e were small (≈ 40 × 40 μm to ≈ 300 × 300 μm) and most were mixed with the embedding material.
More calcified nodules were seen in the mineral map obtained with the 40 × 40 μm spatial resolution than in the 80 × 80 μm map, suggesting that many islands were smaller than 80 × 80 μm and may be even smaller than 40 × 40 μm, as was seen subsequently in the SEM/SDD-EDS Ca and P maps.
Note that many islands of this size range were seen in the FTIR-RM mineral map of the same specimen (Calc2) when mapped with 40 × 40 μm spatial resolution and in the SEM/SDD-EDS P, Ca, Na and Mg maps.
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These included optical sensors viz. a panchromatic stereo camera for terrain mapping (TMC) and Hyper spectral sensors (HySI, SIR-2 and M3) for mineral mapping.
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