基本释义:

原地壳

网络释义

1)protocrust,原地壳

2)Original crust of the Earth,原始地壳

3)lower crust of Qinghai-Tibet plateau,青藏高原下地壳

4)Protoconch

['pr?ut?,k?nk],原壳

5)monitoring of diastrophism in the Qinghai-Xizang plateau,青藏高原地壳运动监测

6)"Original rock formation" of lower crust,下地壳"原始岩石层"

用法和例句

3-D Velocity Structure of the Crust and Upper Mantle in Tibet and Its Geodynamic Effect;

青藏高原地壳上地幔三维速度结构及其地球动力学意义

Numerical Simulation for Displacement of Crustal Movement in Tibetan Plateau and Stress, Strain Analysis Constrained by GPS Data;

GPS约束下青藏高原地壳运动位移场模拟及应力应变分析

Displacement Back Analysis Model and Dynamic Simulation on the Crustal Deformation of Qinghai-Tibet Plateau;

青藏高原地壳形变位移反分析模型及其动态仿真研究

High-Resolution Characteristics of Recent Crustal Movement in Qinghai-Tibet Plateau

青藏高原现今高分辨率地壳运动特征

DETERMINATION OF THE ORIENTATION OF THE CRUSTAL STRESS !N CENTRAL HEBEI PLAIN BY BOREHOLE BREAKOUT METHOD

用孔壁崩落法测定冀中平原地区地壳应力方向

The Crustal Shortening and Reconstruction of the Main Terranes Though Mesozoic-Cenozoic in Qinghai-Tibet Plateau

青藏高原主要地体中新生代地壳短缩作用与地体复原

native to Australia; introduced elsewhere to control scale insects.

原产于澳大利亚；为控制介壳虫引入其它地区。

Application of Convex Hull in Identifying the Types of Urban Land Expansion;

凸壳原理用于城市用地空间扩展类型识别

It is the earth's 40 mile deep crust with which we are concerned when we seek the cause of earthquake.

若我们寻求地震的原因，这40英里地壳恰恰是我们关心的地带。

The Seismic Tomography on the Velocity Structure of the Crust and Upper Mantle in the Northeastern Margin of the Qinghai-Tibetn Plateau

青藏高原东北缘地壳上地幔速度结构的地震层析成像研究

as the basic form of the crust of the earth,

看作地壳的基本模壳，

The upwelling of the mantal substance along fractured zones may be the reason causing the abnormal crust and mantal structure.

地幔物质沿断裂带上涌，可能是形成异常壳幔结构的原因。

The Regional Crustal Stability in Hebei Plain and Its Fuzzy Mathematics Comprehensive Assessment;

河北平原区区域地壳稳定性及其模糊数学综合评价

To teach the law of the crustal movement by the dialectical materialism

用辨证唯物主义的基本原理去讲授地壳运动的规律

] Oceanic-continental crust boundary

大洋地壳与大陆地壳边界

With the development of the crust and its continents, a recognizable ancestor of our present earth appeared.

随着地壳和它的大陆的演变，我们现在的地球的可辨认原型就出现了。

DIFFERENCES OF CRUSTAL STRUCTURES IN NORTHEASTERN EDGE OF TIBET PLATEAU, ORDOS AND TANGSHAN EARTHQUAKE REGION IN NORTH CHINA-RESULTS OF DEEP SEISMIC SOUNDING

青藏高原东北缘、鄂尔多斯和华北唐山震区的地壳结构差异——深地震测深的结果

However, the crust is almost four times thicker than the earth's crust.

然而，月球地壳几乎是地球地壳厚度的四倍。