monoclinic system

It belongs to the monoclinic system and is part of the P21/c group.

They crystallise in the monoclinic system and are green in colour.

Huttonite crystallizes in the monoclinic system with space group P2/n.

It belongs to the monoclinic system with space group C-Cm.

It is a soft yellowish white mineral which crystallizes in the monoclinic system.

It crystallizes in the monoclinic system and forms prismatic crystals.

Epidote group minerals crystallise in both the orthorhombic and monoclinic systems.

Phase I belongs to the P21/n space group of the monoclinic system, with four molecules per unit cell.

The monoclinic system includes crystal classes with a single twofold rotation axis and/or a mirror plane.

Scorzalite crystallizes in the monoclinic system in a dipyramidal form.

The most common crystallization of LiTiO is a monoclinic system.

It crystallizes in the monoclinic system and occurs as white fumarolic encrustations on lava.

A monoclinic system of crystallization is defined as three unequal axes with one oblique intersection.

It crystallizes in the monoclinic system with the chemical composition PbSbS.

The unit cell for the monoclinic system has a base which is a rhombus, with sides a and c inclined at angle β.

It occurs as soft, white clusters of fibrous crystals and encrustations which crystallize in the monoclinic system.

Brazilianite is a mineral in the monoclinic system that is part of the point group 2/m and belongs to the space group P21/n.

Leadhillite crystallises in the monoclinic system, but develops pseudo-hexagonal forms due to crystal twinning.

Thallium carbonate, T12CO3, crystallizes in the monoclinic system, space group C2/m.

Muscovite - The common or white mica; for the most part an orthosilicate of aluminium and potassium, crystallising in the monoclinic system.

Pigeonite crystallizes in the monoclinic system, as does augite, and a miscibility gap exists between the two minerals.

In the monoclinic system, the crystal is described by vectors of unequal lengths, as in the orthorhombic system.

Alloclasite crystallizes in the monoclinic system and typically forms as columnar to radiating acicular prismatic clusters.

Leadhillite belongs to the monoclinic crystal class 2/m, which is the class with the highest symmetry in the monoclinic system.

Crystals of this complex have been shown by X-ray diffraction crystallography to belong to the Cc space group of the monoclinic system.