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等轴砷锑钯矿(Isomertieite)是近年来发现的一种铂族元素新矿物。英国学者Clark及我国于祖相等于1974年分别报道了该矿物的发现。在于祖相的报道中将它称为“丰滦矿”(Fengluanite)。彭志忠等人曾详细地论述了丰滦矿及等轴砷锑钯矿的关系,证明它们确属同一矿物。由于于祖相等同志的文章发表稍晚于英国学者,而且在化学式、粉末图指标化及空间群确定方面有错误,“丰滦矿”的命名未获得国际新矿物及新矿物命名委员会的通过。故现在我们仍将它称作为等轴砷锑钯矿。
Isomertieite is a new platinum group element discovered in recent years. Clark, the British scholar, and Yu Zu, an equal member of China, reported the discovery of the mineral in 1974 respectively. It is called “Fengluanite” in his ancestral report. Peng Zhizhong and others have discussed in detail the relationship between the Fengluuan Mine and the equiaxed arsenic-antimony-palladium mine, proving that they are indeed the same mineral. Due to the publication of later articles by fellow comrades in Britain on British scholars and the mistakes in the chemical formula, powder charting and space group determination, the designation of “Fengluuan Mine” has not been approved by the International Commission of New Mineral and New Mineral Names. So for now we still call it an equiaxed arsenic antimony palladium ore.