XVIIIlea
XVIIIlea is a rare aluminosilicate mineral described from hydrothermal veins in ultramafic rocks of the fictional XVIII Basin in the Lyria Province. Named for the eighteenth district of the XVIII project and using the common mineral suffix -lea, XVIIIlea is considered a distinctive, though scarce, member of its mineral group. It forms colorless to pale blue crystals with a vitreous to silky luster and has a Mohs hardness around 6.5. Crystallographically, XVIIIlea is reported to crystallize in the monoclinic system, typically as prismatic to tabular crystals with a translucent to transparent appearance.
XVIIIlea was first described in 2042 by a collaborative expedition led by researchers including Dr. A. R.
XVIIIlea occurs in hydrothermal veins within ultramafic host rocks and is commonly associated with serpentine, chlorite,
To date, XVIIIlea is known from a single, well-documented locality in the XVIII Basin. Its rarity means
Researchers study XVIIIlea for insights into low-temperature alteration processes in ultramafic environments and for potential dielectric