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 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。
• 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。
• The homogeneous domains were divided within the typical area by considering homogenity of the main structural foliation, among these 8 domains(ⅰ~ⅷ) were selected for detailed SFL π fabric analysis.
  按照主构造面均匀性法则，划分了构造均匀区段，并对其中8个区段（Ⅰ～Ⅷ）进行了详细的SFLπ组构分析。
• 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。
• In structural geology analysis, fabric analysis of foliation and lineation is commonly conducted.
  在构造解析中，对地质构造的面理和线理进行组构分析，往往要涉及到求解赤平图中的极密中心产状和最佳拟合π圆。
• 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；
• Steep mylonite foliation in the later shear belts strikes NE-NNE, and mostly dips SE. Its stretching lineation is gentle and dips SSW, the maximum dip angle is less than 20 °.
  晚期剪切带糜棱面理优势走向为NE-NNE，面理倾角较陡，以向SE倾为主，拉伸线理一致向SSW缓倾，倾角最大不超过20°。
• 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 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 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。