Microstructures of common polygonal serpentines from axial HRTEM imaging, electron diffraction, and lattice-simulation data

被引:25
作者
Baronnet, A
Devouard, B
机构
[1] CNRS, CRMCN, F-13288 Marseille, France
[2] Univ Clermont Ferrand, CNRS, UMR 6524 OPGC, Dept Sci Terre, F-63038 Clermont Ferrand, France
关键词
serpentine-group minerals; polygonal serpentine; microstructure; HRTEM; electron diffraction; dislocation; fast Fourier transform;
D O I
10.2113/gscanmin.43.2.513
中图分类号
P57 [矿物学];
学科分类号
070901 [矿物学、岩石学、矿床学];
摘要
Imaging with high-resolution transmission electron microscopy (HRTEM), selected-area electron diffraction (SAED), and numerical simulations of the diffraction patterns are combined to further document the microstructures of the most widespread types of 15-sector and 30-sector polygonal serpentines. Imaging, diffraction and simulation data recorded along the fiber axis are reconciled with a model involving lateral continuity of the 1: 1 layer structure and a curvature without inversion of the sheets of tetrahedra across the sector boundaries. Axial fivefold symmetry is confirmed for polygonal serpentines. This model differs from sharp-boundary models proposed by Chisholm (1991, 1992), without inversion, and by Dodony (1993, 1997a), with inversion. Streaked diffraction chords connecting Bragg reflections are typical of all polygonal fibrils. They are due to curved layers with constant curvature at sector boundaries, involving extra spacing and locally distorted H-bonds between layers. This is a peculiarity of polygonal serpentines, not present in other varieties of rolled serpentine.
引用
收藏
页码:513 / 542
页数:30
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