【摘要】 绿泥间蜡石是1988年发现的规则混层新矿物。笔者用高温X射线衍射分析方法,将其进行系统实验研究,阐明该矿物在不同温度状态下晶体结构发生的变化情况及其相变时的温度。以及产生的新物相。实验结果显示绿泥间蜡石的相变温度在900℃左右。当温度继续上升,样品中产生了新物相——莫来石。更多还原

【Abstract】 Lnnijanlaite is a new reqular interstratified minera which was found in 1988 in Zhejiang （ and appronroved by IMA in 1990 ） The paper introduces the testing on Lunijianlaite — a new regular interstraiified mineral by the high temperature X-ray diffractometer: declaring the parocedure of changing under high temperature and the phase transition temperature and getting the new phase. The experiment result shows that transition temperature of Lunijianlite is about 900℃ and with the increase in temperature, the new phase formd is Mullite （ 3Al₂O₃·2SiO₂ ）更多还原