foliated
英 [ˈfəʊlɪeɪtɪd]
美 [ˈfoʊliˌeɪtɪd]
v. 把……打成箔；加叶饰; 生叶
foliate的过去分词和过去式
过去式：foliated
英英释义
adj
- (especially of metamorphic rock) having thin leaflike layers or strata
- ornamented with foliage or foils
- foliate tracery
- a foliated capital
双语例句
- The foliated garnet-bearing granites have the geochemical characteristics of A-type granites, suggesting that the magma of these granites in the UHP and HP metamorphic rocks were derived from the partial melting of the retro-metamorphosed UHP metamorphic rocks exhumed into the middle to lower crust.
结合面理化（含榴）花岗岩具有A型花岗岩的地球化学特征分析，它们的岩浆物质可能来自超高压变质岩折返至中下地壳的减压退变和部分熔融。 - Grain size refinement by dynamic recovery and recrystallization is thought to be responsible for the formation of foliated fault locks.
由动态恢复和动态重结晶控制的矿物颗粒的细粒化被认为是产生这些片理化断层岩的原因。 - An ornament at the top of a spire or gable; usually a foliated fleur-de-lis.
在一个尖顶或者山形墙顶上的装饰品；通常由德国的叶状锂构成。 - The experimental results show that weak plane of foliated rocks has a marked effect on rock ultimate strength.
试验结果表明，层状岩石的弱面对岩石的强度值有明显的影响。 - Clusters of water molecules coexisting with dense dislocations indicate that the dominant deformation mechanism of the elongated garnet in foliated eclogite is hydrolysis weakening dislocation glide.
并且有水分子团与高密度位错共存，表明主导石榴石发生强烈塑性变形的机制为水弱化的位错滑移。 - Geometry, kinematics and tectonic implication of the deformed garnets in the foliated eclogite from the ultra high pressure metamorphic belt in the Dabie Mountains, eastern China
大别山超高压变质带面理化榴辉岩中变形石榴石的几何学和运动学特征及其大地构造意义 - 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。 - A banded or foliated metamorphic rock, usually of the same composition as granite. CONTRASTING ARCHAEAN GRANULITE FACIES ROCKS FROM EASTERN HEBEI, NORTH CHINA
片麻岩层状或叶片状变质岩，成分通常与花岗岩相同冀东太古代高级变质地体中两类麻粒岩相深成片麻岩 - I think the foliated rocks within the belt are mostly mylonite.
我认为在这个片理化带中的大多数岩石都是糜棱岩。 - In the Dabie Sulu UHP metamorphic belt, eclogites and meta mafic and ultramafic rocks are characterized by a boudin or lenticular style on all scales from a few centimetres to kilometres, and are enveloped in a regional amphibolite facies gneiss matrix and foliated garnet bearing granitic rocks.
在大别苏鲁超高压变质带内，榴辉岩及变质的镁铁质超镁铁质岩石，一般成厘米至公里尺度的布丁或透镜体，散布于片麻岩及面理化含榴花岗岩内。