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即使变质岩中的片理以及辉长岩中的条带也可产生弯曲而形成褶皱。Even foliated metamorphic rocks and banded gabbro can BE curved to form folds.

分析片理面对二云石英片岩蠕变的影响。Then, the effects of schistosity planes on creep laws of mica-quartz schist are analyzed.

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除此之外，是否具有片理构造是划分断层岩的另一个因素。In addition, the presence and absence of foliation are an other factor to classify fault rocks.

与各向同性相差很大的情况往往产生于层理，片理，某些时候则由于断裂所造成。Macroscopic deviations from isotropy occur due to bedding, schistosity and also sometimes fracturing.

而由云母片岩蚀变而来的绿泥石矿石呈块状或片理状、颜色为灰绿色和深灰色。Massive pyrite-clear quartz ores and network polymetallic sulfide minerals-grey colour quartz ores formed.

在片理面上发育有强烈的拉伸线理，这些线理则是由拉长的矿物定向展布而显示。On the surface of foliation there develops strong stretching lineation defined by alignment of elongated minerals.

在后背与两侧部位，其成型比前片理柔韧，并且不延伸到腰部。On the back and side sections, the shaping is more pliable than on the front and does not extend into the waist area.

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晚期的钠质角闪石构成了现存片理，可能与后期构造变形有关。While, the sodium amphibolites in the later stage compatible with the present foliation , might be related to the structure deformation.

珠光体球墨铸铁轧辊是在球墨铸铁中加入镍、铬、钼合金元素，经过特殊热片理得到珠光体球铁轧辊。Pearlitic nodular rolls are obtained by adding alloy elements of Ni, Cr, Mo into the nodular cas iron and following special heat treatment.

片岩斜坡中弯曲倾倒变形是通过密集的片理上逐层剪切位移实现的。The bending and toppling deformation in slopes of mica quartz schist occurs due to shear displacement slice by slice of schist with concentrated schistosities.

主要容矿构造为剪切带和褶皱，其类型有轴面劈理型、片理型和滑脱面型，矿体组合样式有斜列式、“S”形和“乡”字形、“H”形及网格形等。Structures controlling the orebodies include plane cleavage, schistose cleavage and decollement plane, and the orebodies usually arrange in the form of "S", "H" or grid, and so on.

变质核杂岩的变形片理、线理及运动指向说明该变质核杂岩为对称型变质核杂岩。The metamorphic core complex is considered to be symmetric type metamorphic core complex in the light of deformation schistosity, lineation, and the indication of the shear movement.