stabiileina

Stabiileina is a fictional mineral species introduced as a case study in speculative mineralogy. It is described as a hydrated aluminosilicate with a layered framework that yields high thermal stability and low solubility in acidic media. The mineral is typically pale blue to green, with a vitreous to pearly luster and a Mohs hardness around 4 to 5. Its refractive index is approximately 1.58–1.62, and it shows perfect cleavage in one direction.

The name Stabiileina is derived from the Latin stabilis, meaning stable, combined with the diminutive suffix -eina to indicate small, unit-layered crystals. The species was first described by geologist Elena Voss in 2012, in a hypothetical rock sequence from an alpine metamorphic belt. The description appeared in speculative mineralogical literature and has since circulated in educational discussions about crystal chemistry and phase stability.

In genesis, Stabiileina is theorized to form under high-temperature, high-pressure metamorphic conditions where aluminum-oxygen and silicon-oxygen sheets stack with alkali interlayers. Natural occurrence is said to be localized to ultra-high-temperature schists in the central Alps within the model framework; it is not known to exist in real-world samples outside hypothetical contexts.

Applications in thought experiments include illustrating lattice stabilization mechanisms, buffering effects of interlayer cations, and potential ceramic or catalyst research in controlled laboratory simulations. Current status remains fictional, serving as an illustrative example rather than a confirmed mineral.