Crystal structure of an authigenic maximum microcline
Crystal structure of an authigenic maximum microcline
复制标题
自生最大微斜长石的晶体结构
DOI：
10.1524/zkri.1964.119.5-6.413
复制
发表时间：
1964
期刊：
影响因子：
--
通讯作者：
S. W. Bailey
中科院分区：
文献类型：
--
作者：
J. J. Finney;S. W. Bailey
瑞士Pontiskalk石灰岩中自生最大微斜长石的结构已通过全矩阵最小二乘程序使用797个观测反射和207个未观测反射被细化到δ值为8.5®/n。四面体Si、Al原子的有序化基本完成，与火成最大微斜长石结构无明显差别。晶体被认为在完全有序相的稳定性范围内的低温下生长非常缓慢。
The structure of an authigenic maximum microcline from the Pontiskalk limestone, Switzerland, has been refined to an Ä value of 8.5®/„ by a full-matrix least-squares program using 797 observed and 207 unobserved reflections. The ordering of tetrahedral Si,AI atoms is nearly complete and there is no significant structural difference from an igneous maximum microcline. The crystal is considered to have grown very slowly at a low temperature within the stability field of the fuUy ordered phase.