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Ferrimolybdite : ウィキペディア英語版 | Ferrimolybdite
Ferrimolybdite is a hydrous iron molybdate mineral with formula: Fe3+2(MoO4)3·8(H2O)〔 or Fe3+2(MoO4)3·n(H2O).〔 It forms coatings and radial aggregates of soft yellow needles which crystallize in the orthorhombic system. ==Discovery and occurrence== It was first described in 1914 for an occurrence in the Alekseevskii Mine in the Karysh River Basin, Khakassia Republic, Siberia, Russia.〔 It was named for its composition (ferric iron and molybdenum). It occurs as an oxidation product of molybdenum bearing ore deposits. Associated minerals include: molybdenite, pyrite and chalcopyrite.〔
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Ferrimolybdite」の詳細全文を読む
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