foliation

英

美 [ˌfoʊliˈeɪʃən]

n.  制箔；涂箔；分成薄片；分层；成片；叶理，剥理；（幼）叶卷叠式

复数：foliations　

英英释义

noun

• the work of coating glass with metal foil
• the production of foil by cutting or beating metal into thin leaves
• (architecture) leaf-like architectural ornament
  Synonym:foliage
• (geology) the arrangement of leaflike layers in a rock
• (botany) the process of forming leaves
  Synonym:leafing

双语例句

• The fold in the Xiaoqinling terrane included the outcrop fold and macrofold, and the foliation formed by the fold was the secondary structural foliation.
  小秦岭地体中的褶皱包括露头褶皱和宏观褶皱，组成褶皱的面理为次生构造面理。
• The foliated rock belt is over one hundred meters in width and the intensity of foliation in the center is stronger than that in the margin.
  这个片理化岩带有100多来宽，带中央岩石的片理化程度较之于带边缘岩石要强。
• The change of magnetic fabrics reflects that the ductile deformation in the field is strong in the north and weak in the south, the ductile faults have the features of flattening strain and the attitude of the magnetic foliation is consistent with that of the ductile faults.
  磁组构特征的变化明显反映出矿田韧性变形具北强南弱的特点；矿田韧性断裂具有压扁应变的特征，磁面理产状与韧性断裂产状相一致。
• The magnetic lineation and magnetic foliation study of the ore area show that the magnetic fabric study can proclaim the stress field of rock deformation as the petrofabric analysis.
  矿区的磁线理、磁面理等磁组构研究表明，磁组构能与岩组研究一样，解决岩石变形的应力场问题。
• The early ductile shearing ( DF_1), which is associated with regional D_2 deformation, is accompanied by the growth of synkinematic blueschist-facies minerals including glaucophane, garnet, epidote and phengite etc. with the development of a transposition foliation.
  其中早期韧性剪切变形（DF1）与区域D2变形幕有关，蓝闪片岩相矿物（蓝闪石、石榴子石、绿帘石和多硅白云母）是伴随变形叶理生长的同构造产物。
• Foliation, bloom, and production became erratic.
  萌芽、开花和结果变得很不正常。
• 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。
• These rocks are lack of foliation and resulted from the brittle fragmentation of mineral grains with rotation of grain fragments accompanied by fractional grain boundary sliding and dilatancy.
  这类岩石缺乏面理构造，是由于矿物颗粒的脆性碎裂，旋转以及颗粒边界的磨擦滑动和扩展而造成的。
• The regional foliation and Songyuan anticline were formed by deformation D2. The foliation of rocks does not represent the original stratification and belongs to axial foliation.
  D2期形变造就了区域性宏观面理构造和松源复背斜，岩石面理产状不代表原始沉积层理，属轴面叶理。
• The influence of bound condition on the trend of foliation and high stress area.
  约束条件与层理分布和应力集中区的关系。