The formation of crenulation cleavage
The formation of crenulation cleavage
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圆齿解理的形成
DOI：
--
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发表时间：
1976
影响因子：
2.7
通讯作者：
J. Cosgrove
中科院分区：
文献类型：
--
作者：
J. Cosgrove
对各向异性材料的屈曲理论的研究使矿物织物的微折叠得到了更清楚的理解。结果表明，“微褶皱”与各种屈曲不稳定性有关，这些屈曲不稳定性发生在应力矿物织物或细层压多层材料中。微褶层的发育与应力梯度密切相关，矿物在应力梯度作用下迁移，从而形成微褶层解理面。
Investigation of a theory of buckling of an anisotropic material has enabled the micro-folding of mineral fabrics to be more clearly understood. It is shown that “Crenulations” (microfolds) are associated with a variety of buckling instabilities which develop in stressed mineral fabrics or finely laminated multi-layers. Crenulation cleavage planes are generally formed as a consequence of mineral migration which occurs in response to stress gradients intimately associated with the developing microfolds.