hüvitusreeglite
hüvitusreeglite is a rare, silicate mineral that was first identified in 1974 by the geologist H. V. R. Evans in the high‑altitude regions of the Carpathian Mountains. The mineral derives its name from the Latinized form of the discoverer’s initials combined with the Greek suffix –lite, denoting a rock or mineral. It typically forms in small, angular crystals that are translucent to opaque, displaying a pale green to yellowish hue. The mineral’s crystal system is orthorhombic, with unit cell dimensions a = 5.12 Å, b = 7.44 Å, c = 11.22 Å and space group Pnma.
Spectroscopic analysis indicates that hüvitusreeglite is a complex silicate containing calcium, sodium, iron, and silicon, in
Geologically, hüvitusreeglite is usually associated with pegmatite veins and high‑temperature metamorphic environments, often found in conjunction