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Crystallographic Analysis of the Garnet Structure Type: Symmetry in the Structural Anatomy


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Abstract

The crystallographic analysis of the garnet structure type (Al2Ca3(SiO4)3, Ia3d symmetry) establishes the determining role of the [AlCa6Si6] cation group with the local symmetry \(\bar 3\)in the structure formation. The glide planes of three directions coherently assemble these groups. High structural stability (three not symmetry-fixed coordinates per 80 atoms, the fundamental volume V*~17 Å3) promotes the occurrence of various atomic compositions in it. The relation with the β-W structure type and the structure of menezesite mineral is shown.

About the authors

S. V. Borisov

Nikolaev Institute of Inorganic Chemistry, Siberian Branch

Author for correspondence.
Email: borisov@niic.nsc.ru
Russian Federation, Novosibirsk

S. A. Magarill

Nikolaev Institute of Inorganic Chemistry, Siberian Branch

Email: borisov@niic.nsc.ru
Russian Federation, Novosibirsk

N. V. Pervukhina

Nikolaev Institute of Inorganic Chemistry, Siberian Branch

Email: borisov@niic.nsc.ru
Russian Federation, Novosibirsk

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