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
- 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 properties of a riemannian foliation with parallel mean curvature on a Riemannian manifold;
利用反调和平均曲率流,提出一种各向异性、快速的不规则三角网格去噪算法。 - Foliation is particularly pronounced.
叶理特别发育。 - 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。 - 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; - 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。 - 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。 - 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。