crust的例句大全

The crust and the very top part of earth's next layer, the mantle, are divided into huge sections, called plates.

地壳和地球下面的地幔的顶部，分为巨大的块，叫做板块。

Love wave group dispersion and three dimensional structure of the Pacific crust and upper mantle

勒夫波群速度频散与太平洋地壳及上地幔三维构造

Three-dimensional velocity structures of the crust in West China

中国西部及邻区的地壳三维速度结构

Three-dimensional P velocity structure of the crust and upper mantle under Beijing region

华南上地幔P波速度结构北京地区地壳和上地幔的三维P波速度结构

The analysis of seismic phases in a three-layer model and the structure of the crust

三层介质模型震相分析与地壳结构

Whereas the crust on the southern side has a three-layer structure and there is also a low-velocity layer.

南侧地壳为三层结构，同时有低速度层发育。

Under the same destruction percentage moss crust has the highest threshold velocity, followed by lichen crust, algal and algal-lichen crusts in succession.

相同破损率条件下，起动风速以苔藓结皮最大、地衣结皮次之、藻结皮和藻类地衣结皮最小。

It is thought that millions of years ago this liquid mass pushed upward through cracks in the earth's crust. As the liquid cooled, the carbon charged into diamond crystals.

据认为在数百万年以前，这种液态的物质冷却以后，纯碳就变成了钻石结晶。

Thrust fault zones, as important structures exit in the earth crust, their kinematics characteristic and the geometric deformation is always a hotspot in geology field.

逆冲断裂带作为地壳中普遍存在的重要构造，其运动学特征和几何变形一直是地质学领域的研究热点。

The ultra-high pressure metamorphic belt was uplifted rapidly by obduction to the middle crust in the process of continuous subduction-obduction in the collisional tectonic setting, so it was an allochthon thrust on the subducted basement of the Yangtze plate.

超高压变质带形成于扬子和中朝板块大陆碰撞的构造环境，是扬子板块陆壳向北俯冲到一定深度的变质产物。

Late Yanshan stage was compressive crust deformation which not only formed the wedge-type thrust structure but also caused upper Cretaceous Series unconformable contact with lower Cretaceous Series.

燕山晚期地壳以挤压逆冲变形为主，不仅形成了楔冲式推覆构造，也使上白垩统与下白垩统为角度不整合接触。

The crust movement rate range of coast that distributed tide-gauge stations is 4 4~ 4 1 mm/ a by comparing the sea level change rate of each tide gauge station with the average rising rate of global sea level.

由各验潮站海平面的升降速率与全球海平面平均升高速率比较，得到验潮站所在海岸地壳升降速率在44～-41mm/a之间。

Due to multi cyclical extrusion, strike slip and extension since Mesozoic Cenozoic, the North China Platform was separated and the crust was thinned, and some rift basin constituted by a series of tilt block were formed.

中新生代以来，多旋回的挤压、走滑与伸展作用，使华北地台解体，地壳薄化，并形成由一系列掀斜断块组成的裂谷盆地。

The earth crust in Nanling experienced three time opening closing with different scales;

南岭地区地壳经历3次不同规模的南北向开合活动；

The industrial enrichment of Cu-Ni sulfide needs a relatively stable structure environment, and the long-time movement of structures makes ore magma invade into the shallow crust, gives rise to better crystallization, gravity differentiation and liquation of sulfides and silicates, and further forms ores.

硫化铜镍工业富集需要相对稳定的构造环境，构造长期活动，使得含矿岩浆能够上侵到地壳浅部并发生良好的结晶重力分异作用和硫化物硅酸盐熔离作用，并进而富集成矿。

Every time crust movement formed the difference geological unit and many kinds of geological relics. Passing through investigation and basing on the Hunan provincial concrete conditions, the geological relics of Hunan are divided into 7 kinds and 20 species.

历次的地壳运动，造就了不同地质单元和多种地质遗迹，通过调查，并根据湖南省的实际情况，将湖南省地质遗迹分为7大类20种。

The investigation of the earth structure, especially the crust and upper mantle structure from seismic travel time and waveform data is one of basic topics of seismology.

利用地震波的走时及波形数据研究地球深部结构，特别是地壳上地幔结构，是地震学的一个基本课题。

Tin in magma and magmatic hydrothermal solution migrates as forms of tin hydride and tin alloy hydride to shallow crust level which, then are oxidized to tin oxide, tin alloy mineral or combine with S, H 2S, forming tin sulfides.

在岩浆和热液中，锡以锡氢化物、锡合金氢化物迁移至地壳浅部，锡氢化物、锡合金氢化物被氧化成锡氧化物、锡合金矿物，或与硫、硫化氢作用形成锡的硫化矿物。

The tin ore deposits in Tengchong-Lianghe area were formed in the geochemical cycles related to the regenerated granitic magmatism under the convergent and collision process of plates which occurred in the crust with rich lithophile elements contained.

腾冲-梁河地区锡矿床是富亲石元素地壳在板块会聚碰撞作用下与再生花岗岩浆活动有关的地球化学旋回中形成的。

With the tensional process in the crust being more and more accumulated, the closed system turns to be an open one and sulphophile ore-forming elements decreased while lithophile ore-forming elements ( Ti, Fe, V and P) deposited in large quantity.

随着地壳引张作用加剧，从封闭环境转为开放系统，亲硫成矿元素衰退，大量亲氧元素沉淀（Ti、Fe、V、P）。