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1·Foliation is particularly pronounced.

叶理特别发育。

2·Let us keep walking perpendicular to the trend of foliation to get more details.

我们垂直这些片理化岩石的走向穿越一段并作详细观察。

3·The effect of the different stresses on the trend of foliation and high stress area;

差应力大小与层理分布和应力集中区的关系；

4·In addition, the presence and absence of foliation are an other factor to classify fault rocks.

除此之外，是否具有片理构造是划分断层岩的另一个因素。

5·I think the foliation is resulted from deformation. The original composition of the foliated rock is granite.

我认为岩石中的这些片理是由于岩石变形造成的，片理化岩石的原岩就是花岗岩。

6·On the surface of foliation there develops strong stretching lineation defined by alignment of elongated minerals.

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。

7·In particular, the space is characterized by horizontal distribution of projective sphere bundle to have flat foliation.

特别地，这个空间可以由摄影球丛具有平坦的叶状结构的水平分布来刻划。

8·While, the sodium amphibolites in the later stage compatible with the present foliation, might be related to the structure deformation.

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。

9·Foliated fault rocks are characterized by well-developed foliation which is resulted from the preferred orientation of mineral grains in the rock.

片理化断层岩石具有发育良好的面理构造，这些面理是岩石中矿物颗粒优选定向而造成的。

10·Strong foliation, stretching lineation, a-type folds, sheath folds and mylonite, these structural characteristics only reflect macroscopic evidence.

强烈的片理、拉伸线理、a型褶皱、鞘褶皱以及糜棱岩，这些构造特征仅仅反映出宏观的证据。

叶理

1·This paper introduces the method for a strain analysis of the fabric (foliation and lineation) of granite by using the theory of the strain ellipsoid.

本文介绍了利用变形椭球体理论，对花岗岩组构(叶理、线理)进行应变分析的方法。

2·Foliation is particularly pronounced.

叶理特别发育。

3·In most cases, the deformed rocks within ductile shear zones are mylonites, because rock grain size obviously reduced and strengthening foliation (lineation) developed.

在大多数情况下，韧性剪切带中的变形岩石为糜棱岩，因为经受韧性剪切变形时，岩石的粒度显著减小并发育了强化的叶理(线理)。