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
- In particular, the space is characterized by horizontal distribution of projective sphere bundle to have flat foliation.
特别地,这个空间可以由摄影球丛具有平坦的叶状结构的水平分布来刻划。 - 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 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。 - 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。 - The attitude of magnetic foliation, which clearly suggests the emplacement of the magma in different tectonic units, is consistent with rock shapes and distribution of rock units.
磁面理的产状与岩体形态和岩石单元分布相吻合,清晰地反映了不同构造单元岩浆侵位方式; - 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°。 - 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 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 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。 - 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。
