Compounds of the crandallite type comprise a natural mineral group reaching from proper crandallite CaAl 3(OH) 6(HPO 4)(PO 4) over woodhouseite CaAl 3(OH) 6(SO 4)(PO 4) to alunite KAl 3(OH) 6(SO 4) 2.
纤磷钙铝石类化合物系由自纤磷钙铝石CaAl3 (OH) 6(HPO4) (PO4)本身、经磷钙铝石CaAl3 (OH) 6(SO4) (PO4)到钾明矾石KAl3 (OH ) 6(SO4) 2 等的天然矿物族所组成的。
The main conditions of phase transformation of whitlockite to its high-pressure polymorph, tuite, in the shock melt veins of the Suizhou meteorite, were investigated using microbeam mineralogical techniques and Raman spectroscopy, and combined with the experimental study at high pressures and temperatures.
用微束矿物学和激光拉曼光谱等分析测试技术,并结合人工高压实验结果,研究了我国随州陨石冲击熔脉中的白磷钙石高压相变形成涂氏磷钙石的必要条件,并对寺巷口陨石冲击熔脉中的白磷钙石虽与林伍德石、镁铁榴石和玲根石等高压矿物共生,但仅表现为结构损伤而未相变成涂氏磷钙石的原因进行了探讨。
It is identified as a high pressure polymorph of whitlockite.
在随州陨石冲击熔脉中发现了一种磷酸盐新矿物,它是白磷钙石的高压多形,经国际矿物协会新矿物和矿物命名委员会批准,定名为涂氏磷钙石(Tuite)。
A study of turquoise and secondary woodhouseite from Yuertan,Baihe County,Shaanxi Province;
陕西白河县月儿潭绿松石与次生磷钙铝矾研究