Monoglütseriidit

Monoglütseriidit is a mineral species within the glütseriidit group of minerals. It is a rare mineral, primarily known for its occurrence in the Khibiny Massif, Russia. The mineral was first described in 1967 and named after its chemical composition, which is based on the element monoglütseride.

The crystal structure of monoglütseriidit is orthorhombic, with a space group of Pnma. It typically forms as an accessory mineral in ultramafic rocks, often associated with other glütseriidit group minerals such as glütseriidit and glütseriidit-(Y). Monoglütseriidit is characterized by its bright yellow to orange-red color, which is due to the presence of iron and other transition metals.

The mineral is not typically found in significant quantities and is often of interest to mineral collectors and researchers due to its rarity and unique properties. Its occurrence in the Khibiny Massif is notable, as this region is known for its diverse and unique mineral deposits.

Monoglütseriidit has not been widely studied, and its exact formation conditions and environmental significance are not fully understood. However, its presence in ultramafic rocks suggests a possible association with magmatic processes and the formation of mafic and ultramafic igneous rocks.

In summary, monoglütseriidit is a rare and interesting mineral with a unique chemical composition and crystal structure. Its occurrence in the Khibiny Massif and its association with other glütseriidit group minerals make it a subject of study for mineralogists and geologists.