lithosphere slab

Based on the concept of lithosphere plate and latitudinal normal density hypothesis,concept of asthenosphere plate is put forward.

根据岩石圈板块概念和地幔对流假说的基本观点、以及“纬向正常密度假说”和“板块运动重力机制”的基本观点,提出了“软流圈板块”概念。

The rule of variation of residual paleomagnetic declination by the drift of lithospheric plate.;

岩石圈板块漂移引起岩石古剩磁偏角变化规律

outward-spreading lithospheric plate

向外扩张的岩石圈板块

Earthquakes along Benioff zones are distributed in the descending lithosphere slabs.

贝尼奥夫带的地震都分布在下降岩石圈板块内。

The existence and movement of large lithospheric plates seems well established.

巨大岩石圈板块的存在与位移似乎已完全确定了。

TECTONIC EVOLUTION OF THE LITHOSPHERE PLATES AND SOME FEATURES OF THE SEDIMENTARY DISTRIBUTION IN CENOZOIC ERA IN SOUTH CHINA SEA

南海新生代岩石圈板块的演化和沉积分布的某些特征

The Earth's lithosphere is formed of a rather small number of major plates.

地球的岩石圈是由少数大板块所组成的。

THE CRUST-MANTLE LITHOSPHERE STRUCTURE ANDTHE PALEOZOIC BASINS ON THE NORTHERNMARGIN OF YANGTZE PLATE

扬子板块北缘壳(慢)岩石圈结构与古生代盆地

The site of this destruction is another kind of plate boundary: a subduction zone.

销毁旧岩石圈的地方形成另外一种板块边界：一块潜没的区域。

The theory of plate tectonics describes the motions of the lithosphere, the comparatively rigid outer layer of the Earth that includes all the crust and part of the underlying mantle.

板块结构理论描述岩石圈的运动。 岩石圈是相对坚硬的地球外层，包括全部地壳和部分地幔。

Notice first that there could be a substantial difference between lithosphere thickness and plate thickness.

首先要注意：岩石圈厚度和板块厚度之间可能有重要区别。

As the plates diverge from a mid-ocean ridge they slide on a more yielding layer at the base of the lithosphere.

当板块从中海脊脱离时，它们滑向在岩石圈基部较易变形的地层上。

Lithospheric Thermotectonic Simulation on the Indian-Eurasian Subduction and Collision

印度与欧亚板块俯冲-碰撞过程岩石圈热结构模拟

GRAVITY ANOMALIES, LITHOSPHERIC STRUCTURE AND PLATE TECTONIC DYNAMICS IN THE HIMALAYAS AND NEIGHBOURING AREAS

喜马拉雅及其邻区的重力异常、岩石圈构造与板块动力模型

Lithophere and the Modern Determination of Its Plate Motion-Primary results for the extension of atlantic ridge

地球岩石圈及其板块运动的现代测定——大西洋扩张的初步结果

The lithosphere is divided into a few dozen plates of various sizes and shapes, in general the plates are in motion with respect to one another.

岩石圈被划分为几十个大小不同形状各异的板块，一般而言这些板块都处于相对运动之中。

A mid-ocean ridge is a boundary between plates where new lithospheric material is injected from below.

一道中海脊是板块之间的边界，在那里新的岩石圈的物质从下部注入。

The rocky crust of the earth.

岩石圈地球的岩石外表

Magmatic Process and Source for the Permian Basic Rocks in the Northeast of Tarim Plate

塔里木板块东北部二叠纪基性岩石的岩浆过程与岩浆源区

Separate rock layers, or plates, under the oceans and continents move very slowly.

海洋和陆地下面的岩石层或板块在缓慢地运动。