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saponite belongs to the smectite group of clay minerals. It has a greasy lustre and is found in a variety of colours from white or cream through to blue, green or red-tinged. Saponite is found as a low-temeprature alteration mineral in hydrothermal mineralized veins; infilling vesicules in basalt; in fissures cutting calc-silicates, iron-rich skarns, amphibolites, and in serpentinite (Anthony et al., 1995). The presence of saponite is generally only confirmed by X-ray diffraction or microprobe analysis.
as with many other low-grade metamorphic and hydrothermally produced secondary silicate minerals there are just a few reported occurrences in the literature. It is however likely that the distribution of such minerals, including saponite, is far wider than is currently documented.