It is first studied for the thermal analysis of phlogopite ─ vermiculite interstratification in this paper.
文中首次对金云母&蛭石间层矿物的热分析谱进行了研究。
That the layer structure of the phlogopite layers and the vermiculite layers are broken down have different tempera-ture points in phlogopite ─ Vermiculite interstratification, The former is between 800 ─ 900 ℃ and the latter is between 900 ─ 1000 ℃.
金云母晶层和蛭石晶层结构破坏的温度点是不同的，前者在800～900℃之间，后者在900～1000℃之间。这为加工生产膨胀蛭石提供了重要的技术参数。
With the increase of the depth, the contents of illite and chlorite increases, while the contents of kaolin and the interstratification of illite and montmorillonite decrease.
随着埋深的增加，伊利石和绿泥石的含量增加，高岭石和伊/蒙混层含量减少。
The phlogopite-vermiculite interstratification mineral samples from the Weli mine of Xinjiang were acidized with hydrochloric acid.
对采自新疆尉犁蛭石矿的金云母蛭石间层矿物样品进行了酸处理实验研究。