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一、前言黑铝镁铁矿(Hgbomite)在自然界比较稀少,系一含Ti的(Mg、Fe)-Al氧化物矿物.其结构同尖晶石,尤其是尼日利亚石及塔菲石密切有关,故结晶化学家将后二者与其归于一组,视为等结构类.该矿物自加维林(1917)报道后在南非、坦桑尼亚、北美的纽约及卡罗来那州,以及苏联的乌克兰和喀麦隆等地相继有过发现.近年来在澳大利亚、坦桑尼亚及赞比亚又找到了一些新产地,但在我国还从未见到有关它的报道.作者对我国最近所发现的富含锡、锌的黑铝镁铁矿新变种进行了初步的研究.
I. INTRODUCTION Hgbomite is relatively rare in nature and is a (Mg, Fe) -Al oxide mineral containing Ti. Its structure is closely related to spinel, especially Nigerianite and taffeta, Crystalline chemists then group the latter two groups into one group, which is considered as an isostructural class. The mineral was reported in Galicia (1917) in South Africa, Tanzania, New York and Carolina in North America, and Ukraine and Cameroon in the Soviet Union Have been discovered in recent years in Australia, Tanzania and Zambia have found some new places, but in our country has never seen any reports about it.The author of our country recently found that rich in tin, zinc, aluminum A new variant of mafic iron was studied.