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袁复礼石是一种Ｍｇ、Ｆｅ３＋、Ａｌ３＋和Ｔｉ的硼酸盐新矿物。除了与遂安石、硬石膏和磷灰石共生外，还与硼铝镁石、镁橄榄石和方解石等共生，形成两个矿物共生组合。单矿物化学分析表明，后一组合中的袁复礼石更富铁，特别是Ｆｅ３＋，相对贫镁。袁复礼石的晶体结构分析证明，袁复礼石与硼钛镁石的结构类型一致，阳离子的占位为Ｍ（１）＝Ｍｅ３＋，Ｍ（２）＝Ｍｅ２＋。袁复礼石是Ｍ（１）位置上为Ｆｅ端员组分，Ｍ（２）位置上为Ｍｇ端员组分的新矿物。
Yuanfuliite is a new borate mineral of Mg, Fe3 +, Al3 + and Ti. In addition to the symbiosis with Sui’an stone, anhydrite and apatite, it is also symbiotic with the baulite, forsterite and calcite to form a symbiotic assemblage of two minerals. A single mineral chemical analysis showed that the later complex, Yuanfu Li Stone, is more iron-rich, especially Fe3 +, and is relatively poor in magnesium. The crystal structure analysis of Yuanfulizi proved that the structure type of Yuanfuliite is consistent with that of borosilicate. The cation occupies M (1) = Me3 + and M (2) = Me2 +. Yuanfuliite is a new mineral with M (1) at the Fe end component and M (2) at the Mg end component.