片理

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。

On the surface of foliation there develops strong stretching lineation defined by alignment of elongate d 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。

Look at this exposure. The rock has well-developed foliation defined by elongated quartz and feldspar parallel to each other.

快看这个露头，这个露头上的岩石具有很发育的片理，片理是由拉长的石英和长石相互平行排列而成

Look at this exposure. The rock has well-developed foliation defined by elongate d quartz and feldspar parallel to each other.

快看这个露头，这个露头上的岩石具有很发育的片理，片理是由拉长的石英和长石相互平行排列而成

There are some small scale folds in the foliated rock. Their fold axial planes are parallel to the foliation and on the surface of folded foliation, the stretching lineation is parallel to the fold hinges.

在这些片理化岩石中有一些小型褶皱，这些小型褶皱的轴面平行片理面，在被褶皱了的片理面上有着平行褶皱枢纽分布的拉伸线理。

A sheath fold looks like a scabbard or human's tongue. Its fold axial plane or flatten ed plane is parallel to the foliation and there is strong stretching lineation on the sheath fold.

鞘褶皱看起来像一把鞘或是像人的舌头，它的褶皱轴面或压扁面是平行岩石中的片理面的，鞘褶皱上有强烈的拉伸线理。

It is, in fact, concerned with foliation, flow surface, schistosity

实际涉及面理、流面、片理、片麻理、劈理和各种破裂面等类型。

Firstly, triaxial compression creep tests with mica-quartzose schist which is a kind of soft metamorphic rock with lots of schistosity surfaces were carried out on the rock servo-controlling rheology testing machine under the condition of the axial stress vertical to the direction of the schistosity surface.

首先，对片理发育的软弱变质岩—云母石英片岩，在轴向力与片理垂直的条件下，采用岩石全自动流变伺服仪进行了三轴压缩蠕变试验，对轴向蠕变和径向蠕变进行了对比分析，提出径向蠕变比轴向蠕变敏感，以径向蠕变长期强度作为长期强度更合理。

Supracrustal sequences free of early strong deformation The early deformation of Jingangku formation complex of Hengshan Wutai group complex has formed a bedding parallel S〓 gneissic and schistosity, occasionally bedding parallel recumbent folds in layers. The early deformation of the near-horizontal ductile shearing isn't very strong in Wutai group complex. The orientation of shear movement is NNW—SSE.

经受早期强烈变形的表壳岩系岩系恒山五台岩群金岗库岩组和五台山五台岩群最早期的变形是平行地层层理的S1片麻理和片理，偶见层内的顺层掩卧褶皱，这些早期近水平韧性剪切变形在五台岩群大都不甚强烈，对地层层序的扰动也很弱，剪切运动方向是北西西——南南东向的。

There are some small scale folds in the foliated rock. Their fold axial planes are parallel to the

在这些片理化岩石中有一些小型褶皱，这些小型褶皱的轴面平行片理面，在被褶皱了的片理面上有着平行褶皱枢纽分布的拉伸线理。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。