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 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。
• 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。
• PaDSZ is characterized by the pimple-shaped phyllites containing "foliation fish" by the contents of which the intensities of rocks are determined.
  前者以含“叶理鱼”的疙瘩状千枚岩为特征，“叶理鱼”的含量决定了其应变强度。
• 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。
• The oil shale on the surface show opening foliation, abundant pore volume and low density because of less overburden pressure.
  地表油页岩由于覆压减小等影响，页理张开、孔隙增加、密度减小。
• 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。
• 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。
• 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°。
• 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。