Continental Crust is the inevitable product of formation and evolution of the Earth.
大陆地壳是地球形成演化的必然产物。
A series of astonishing discoveries including seismic reflective,low velocity layer, and low resistivity layer in continental lower crust suggest that we should recognize continental lithosphere, and approach continental lower crust.
下地壳反射层 (或反射下地壳 )、下地壳低速层和低阻层等一系列惊人发现唤醒我们必须重新认识大陆岩石圈 ,研究大陆下地壳。
The major results about magnetic petrology of high-grade terrenes of Archean shield areas in the world are reviewed in this article,focusing on the relationship between rock magnetism and deformation, and metamorphism and intensity of magnetization of continental lower crust and its origin.
综述国际上有关太古宙高级地体磁性岩石学研究的主要成果,侧重高级地体岩石磁性与变形、变质等级的相互关系及大陆下地壳磁化强度及其成因机制等;提出了有关高级地体岩石磁性研究中值得注意的几个问题。
Continental tectonics is akey frontier that involves following important areas such as the formation and evolution oforogenic belts and sedimentary basins, three-dimension layer-block texture of continentallithosphere,thermal and rheological state of continental lower crust,seismic genesis anddynamic sources of continental crust movement.
大陆构造是大陆动力学的核心领域，涉及到盆地和造山带的形成与演化、大陆岩石圈三维层块结构、大陆下地壳的热状态和流变状态、大陆地震成因和大陆地壳运动的动力来源等一系列重大课题。
] Oceanic-continental crust boundary
大洋地壳与大陆地壳边界
The continental crust is much thicker than average beneath the great mountain belts.
在高山地带下面的大陆地壳，其厚度要比平均厚度大得多。
Tomography for The 3-D S -Wave Quality Factor Q_B Structure of Crust and Upper Mantle in China;
中国大陆地壳上地幔S波品质因子三维层析成像
The Fate of Subducted Continental Crust: An Experimental Study
大陆地壳岩石深俯冲过程中的命运：高温高压实验研究
The convective heat of molten magma in the upper 10 km of the continental crust represents a significant geothermal energy resource.
大陆地壳10公里深度以内熔岩中的对流热是一种重要的地热能资源。
A preliminary study of the relationship between granitoids and the growth of continental crust:a case study of the formation of key orogen granitoids in China
花岗岩类与大陆地壳生长初探——以中国典型造山带花岗岩类岩石的形成为例
Equilibrium in the earth's crust such that the forces tending to elevate land masses balance the forces tending to depress land masses.
地壳均衡地壳的均衡，以使趋向于抬高大陆的力与趋向于降低大陆的力保持平衡
The crust can be divided into two types, oceanic and continental.
地壳可以被分成两类：海洋性的和大陆性的。
Present-day Crustal Deformation in China and GPS-derived Coordinate Time Series Analysis;
中国大陆现今地壳形变与GPS坐标时间序列分析
Rheological Properties of the Continental Lower Crust and Destruction Mechanism of the North China Craton
大陆下地壳流变性质与华北克拉通破坏机制
Old World genus of isopod crustaceans.
陆生等足甲壳类旧大陆鼠妇科的一属。
Uplift or depression of the earth's crust, affecting large areas of land or ocean bottom.
造陆作用对大面积地和海底产生影响的地壳的升起或下陷
Research on the Distribution Rule of the Shallow Crustal Geostress Field in the China Mainland and Engineering Disturbance Characteristics
中国大陆浅层地壳地应力场分布规律及工程扰动特征研究
edible terrestrial snail usually served in the shell with a sauce of melted butter and garlic.
可以食用的陆地蜗牛，常在贝壳里加熔化的奶油和大蒜汁。
The Crustal Deformation Pattern in China Inferred from Global Positionging System Measuremants;
用全球定位系统（GPS）研究中国大陆现今地壳运动模式
However, the crust is not a homogeneous shell in which lower places are filled with water to make oceans and high places piled up with rocks to make continents.
但地壳并不是一个均匀的壳，其低处充满了水并构成海洋，高处堆积着岩石构成大陆。
The land mass comprising the continents of Europe and Asia.
欧亚（大陆）由欧亚大陆构成的陆地块
Violent crust movements always happen near the continental shelf.
陆坡区域的地壳经常出现剧烈的活动。