基本释义:

外张的

网络释义

1)extratensive,外张的

2)outer product of tensors,张量的外积

3)apotaphral,向外扩张构造的

4)a flaring bowl,碗口向外张的碗

5)outward-spreading lithospheric plate,向外扩张的岩石圈板块

6)Zhang Ji's Foreign Ideas,论张洎的外交思想

用法和例句

outward-spreading lithospheric plate

向外扩张的岩石圈板块

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 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。

As the plates perge 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。

The rocky crust of the earth.

岩石圈地球的岩石外表

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。

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。

Discussion on the South China Sea Evolution and Lithospheric Breakup through 3D Analogue Modeling

南海岩石圈破裂方式与扩张过程的三维物理模拟

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 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。

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

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 lithosphere is pided 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。

After dropping a small stone into still water, we saw ripples going out in all directions.

把一块小石头扔进平静的水中，我们看到一圈圈的涟漪向四面八方扩散。

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。

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。

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