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See also:PEROVSKITE, or PEROFSKITE , a See also:mineral consisting of See also:calcium titanate, CaTiO3, usually with a small proportion of the calcium replaced by See also:iron. The crystals found in schistose rocks have the See also:form of cubes, which are sometimes modified on the edges and corners by numerous small planes; on the other See also:hand, the crystals occurring as an See also:accessory constituent of eruptive rocks are octahedral in form and microscopic in See also:size. Although geometrically cubic, the crystals 'are always doubly refracting, and they sometimes show See also:evidence of complex mimetic twinning; their structure as shown in polarized See also:light is very similar to that of the mineral See also:boracite, and they are therefore described as pseudo-cubic. There are distinct cleavages parallel to the faces of the See also:cube. The See also:colour varies from See also:pale yellow to blackish-See also: (L. J. Additional information and CommentsThere are no comments yet for this article.
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