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
- (geology) the arrangement of leaflike layers in a rock
- (botany) the process of forming leaves
双语例句
- 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。 - 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 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。 - Foliation is particularly pronounced.
叶理特别发育。 - 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。 - 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。 - 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 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； - 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。 - 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。