粘土矿物
埃洛石
粉末衍射
六方晶系
矿物
单位(环理论)
结晶学
矿物学
格子(音乐)
化学
材料科学
地质学
地球化学
数学
冶金
物理
数学教育
声学
出处
期刊:Powder Diffraction
[Cambridge University Press]
日期:1989-03-01
卷期号:4 (1): 19-20
被引量:13
标识
DOI:10.1017/s0885715600016249
摘要
Abstract The unit cell dimensions of minerals in the smectite group, regular and random mixed-layer groups, and halloysite shown in the Mineral Powder Diffraction File (1986) have been refined by least-squares analysis in the hexagonal system with a primitive lattice with indices restricted to hk or 00 l reflections. Trioctahedral minerals have larger a unit-cell dimensions than dioctahedral minerals.
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