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锶磷钙铝矾(Strontium Woodhouseite)是磷锶铝矾(svanbergite)和磷钙铝矾(woodhouseite)之间的过渡矿物。国外已先后发现该系列矿物的两个湍元,本文为与其他文献不同的典型的中间矿物。 作者1980年在研究苏州市阳山东白善岭高岭土矿区的物质组成时发现了该矿物。经等离子发射光谱定性分析,该矿物的锶元素含量很高,嗣后进行了x射线粉晶照相,电子探针和能谱定量分析,确定为锶离子比值略低于钙离子比值的锶磷钙铝矾。
Strontium Woodhouseite is a transitional mineral between svanbergite and woodhouseite. Abroad has discovered two series of turbulent elements of this series of minerals, this article is different from other literature typical intermediate minerals. The author discovered the mineral in 1980 when it studied the material composition of the Baishanling kaolin mine in Yangshan, Suzhou City. After qualitative analysis by plasma emission spectrometry, the content of strontium in the mineral was very high. Subsequently, X-ray powder crystallography, electron probe and energy spectrum quantitative analysis were carried out to determine the strontium calcium phosphate aluminum whose strontium ion ratio was slightly lower than the calcium ion ratio alum.