This specimen features a crust of cream-white aggregates of micro crystals identified via X-ray diffraction (XRD) in 2004 as kaolinite, accompanied by calcite and quartz.
Kaolinite is a soft, earthy mineral, usually white, and belongs to the dioctahedral phyllosilicate clays. It forms through the chemical weathering of aluminum silicate minerals such as feldspar. In many regions, kaolin is colored pink-orange-red by iron oxide, giving it a distinct rust hue.
This particular specimen, collected by Dr. Tarassoff in 1977, originates from the Francon Quarry. Known for its alkalic intrusive sill in limestone, the quarry ceased operations in 1981 and will never reopen, making specimens from this location particularly rare and valuable to collectors. The confirmed presence of kaolinite and its associations with calcite and quartz highlight the geological diversity and mineralogical significance of this find.
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