| 高岭石-伊利石-透辉石体系假相图 |
| |
| 引用本文： | 戴长禄,张振禹.高岭石-伊利石-透辉石体系假相图[J].地质科学,1993,28(3):254-261. |
| |
| 作者姓名： | 戴长禄 张振禹 |
| |
| 作者单位： | 中国科学院地质研究所, 北京100029 |
| |
| 摘 要： | 采用较纯透辉石岩、高岭石粘土和伊利石粘土作为端元组分,并根据用 DTA、热台显微镜、XRD 方法测定的数据组成了三元体系的假相图。根据假相图说明了有关陶瓷工艺学和变质岩岩石学的一些问题。
|
| 关 键 词： | 假相图 固相反应 陶瓷 透辉石 伊利石 高岭石 |
| 收稿时间： | 1991-05-01 |
| 修稿时间： | 1991-05-01; |
THE PSEUDOPHASE DIAGRAM OF THE DIOPSIDE-ILLITE (HYDROMUSCOVITE)-KAOLINITE SYSTEM |
| |
| Dai Changlu Zhang Zhenyu Ye BanianWu Meiqing Liu Weiling Guo BezhiZhang Quanchang.THE PSEUDOPHASE DIAGRAM OF THE DIOPSIDE-ILLITE (HYDROMUSCOVITE)-KAOLINITE SYSTEM[J].Chinese Journal of Geology,1993,28(3):254-261. |
| |
| Authors: | Dai Changlu Zhang Zhenyu Ye BanianWu Meiqing Liu Weiling Guo BezhiZhang Quanchang |
| |
| Institution: | Institute of Geology Academia Sinica, Beijing 100029 |
| |
| Abstract: | Using relatively pure diopsidite, tllite-clay and kaolinite-clay as end-member components and the data on lowest eutectic temperature and melting temperature of mixture composed of diopsidite, illite-clay and kaolinite-clay of different weight ratios determined by DTA and hot-stage microscopy and on mineral phase species produced by its heating at different temperatures by means of XRD, the triple pseudophase d iagrams are constructed.The pseudophase diagrams are used to explain some problems concerning with ceramic technology and petrology of metamorphic rocks formed from alumina-rich mudstone or shale. Then seven solid phase reactions between diopside, ildite and kaolinite are proposed. These reactions can be thermodynamically take place. |
| |
| Keywords: | Diopside Illite Kaolinite Pseudophase Diagram Ceramics |
| 本文献已被 CNKI 维普 等数据库收录！ |
| 点击此处可从《地质科学》浏览原始摘要信息 |
| 点击此处可从《地质科学》下载免费的PDF全文 |
