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

• Steep mylonite foliation in the earlier shear belts strikes NE-NNE, and dips NW or SE; its stretching lineation is gentle.
  早期剪切带糜棱面理走向NE-NNE，倾向NW或SE，面理倾角较陡，矿物拉伸线理水平或近水平；
• 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。
• 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 article discussed in detail the ductile shear zone of Xuefeng arc-shaped and Yongzhou-Zhuzhou of NE trend, indicated that strong-straight foliation zone is the basic characteristics of ductile shear zone in middle-low metamorphic rock area.
  通过对雪峰弧形和永州&株洲向韧性剪切带较详细的研究，指出在中浅变质岩区，强直面理化带是韧性剪切带的基本NE特征之一。
• Foliation, bloom, and production became erratic.
  萌芽、开花和结果变得很不正常。
• 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。
• 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 further study on the bedding-sliding structure gains a new understanding for the regional foliation formation closely linked in its genesis to the bed-sliding structure.
  通过对层滑构造的进一步研究，得出区域面理的形成与层滑构造有密切成因联系的新认识。
• Foliation is particularly pronounced.
  叶理特别发育。
• Regional geological study suggests that from east to west the Hercynian-Indosinian granites in Hainan Island show an evolution trend of increasingly younger ages and demonstrate an arc-shaped foliation structure.
  通过区域分析，认为海南岛海西&印支期花岗岩从西往东，具有由老至新的演化规律，形成了略向南面突出的弧状面理构造。