Hagendorfite is in the monoclinic crystal class; the mineral's internal symmetry consists of three axes with unequal length.
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Moreover, the crystals are cubic form with a point group of 4 3m, thus having an isometric crystal class.
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Accordingly, the rest of groups of crystal symmetry where QMR can be observed constitutes 27 antiferromagnetic and 31 pyromagnetic crystal classes.
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Sarabauite is of the 2 / m crystal class; it has a 2 fold rotation axis perpendicular to a mirror plane.
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Its crystal system is monoclinic with possible crystal classes of twofold symmetry, mirror plane symmetry, and twofold with a mirror plane.
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The crystal class is 2 / m, meaning the structure has an hexagonal closest packing of sulfur atoms with a monoclinic space group.
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Crystal class : is a classification by Carl Hermann und Charles-Victor Mauguin ( Hermann Mauguin notation ) or Arthur Schoenflies ( Schoenflies notation ).
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In 1935, Niggli and his doctoral student Werner Nowacki ( 1909 1988 ) determined the 73 three-dimensional arithmetic crystal classes ( symmorphic space groups ).
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Kainosite, is part of the orthorhombic crystal class minerals, which is a system that results from stretching a cubic lattice along two of its orthogonal pairs.
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The trigonal crystal system consists of the 5 point groups that have a single three-fold rotation axis ( see table in Crystal system # Crystal classes ).
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