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- W2029659524 abstract "Fe–deficient nonstoichiometric olivine related minerals, x⁄2Fex3+Fe2−(3⁄2)x2+SiO4 have been identified in samples from many localities in Colorado, U.S.A. and in Japan, where denotes vacancies in the structure. It is possible to classify these Fe–deficient olivine minerals into several crystallographically-distinct species. Laihunite has monoclinic symmetry and this include two superstructures, the laihunite–2M and laihunite–3M types in Ramsdell notation. Laihunite associated with the laihunite–3M superstructure is most commonly found in rock types such as metamorphic rock, migmatite, pegmatite and is, in many cases, accompanied by magnetite. Laihunite associated with the laihunite–2M superstructure was found in dacite and is accompanied by hematite. Fe–deficient manganoan olivine occurs in pegmatites, has orthorhombic symmetry, and is termed as ferri-knebelite in this study in order to distinguish it from other related materials. Based on these results, it can be said that the Fe–deficient olivine minerals are fairly common in many rock types and are widespread in their occurrence." @default.
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- W2029659524 title "Fe–deficient olivine structure type minerals from Colorado, U. S. A. and Japan" @default.
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- W2029659524 doi "https://doi.org/10.2465/minerj.12.376" @default.
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