岩浆

Melt structure plays an important role in governing physical and thermodynamic characteristics of magmas.

熔体结构对岩浆的物理和热力学性质起著重要的制约作用。

Consequently, magmas generated within the mantle must be the result of partial melting .

结果，在地涵里面的产生的岩浆一定是结果部分的熔化。

Magmas in transit to the surface will further supplement this heat.

向地表运移的岩浆将进一步补充这种热量。

Low concentration of compatible elements in all the rocks indicates the magmas experienced different extent of differentiation crystallization.

各期次玄武岩的相容元素丰度较低，表明岩浆发生过不同程度的分离结晶作用。

Our model explains why segregation mainly occurs at particular levels and produces distinctive magmas.

我们的棋式说明了为什么分凝作用主要发生在特定的深度和产生的性质不同的岩浆。

The evidences indicate that the magmas are formed by melting of p...

这说明它们是在地幔柱轴部，由地幔岩和榴辉岩组成的源区产生的岩浆形成的。

Temperatures of most magmas are in the range 700°C to 1300°C, but very rare carbonatite melts may be as cool as 600°C, and komatiite melts may have been as hot at 1600°C.

气温的最岩浆是在射程700 ℃至1300 ℃之间，但非常罕见的碳酸岩熔体，可作为冷静的600 ° c ，以及科马提岩熔体可能已被作为热点在1600摄氏度。

Quantitative modelling shows that the magmas are derived from the upper mantle contaminated by crustal material.

定量模拟表明岩浆来源于受地壳物质混染的上地幔。

R adiogenic isotope ratios can be used as a kind of petrogenetic "DNA" to identify the source components of magmas.

放射性同位素可以用作一种岩石成因的& DNA &来识别岩浆源区的组成。

The redox state of basalt magmas is between those of oxygen buffers FMQ and HM.

玄武岩浆喷发前的氧化状态处于FMQ和HM缓冲剂之间。

However, as the name（read－only memory）implies, CD disks cannot be written onorchanged in any way.

然而，正如其名字所指出的那样，CD盘不能写，也不能用任何方式改变其内容。

Galvanizes steel pallet is mainly export which suits standard packing of European Union, the North America. galvanizes steel pallet is suitable to heavy rack. Pallet surface can design plate type, corrugated and the gap form, satisfies the different requirements.

镀锌钢托盘多用于出口，替代木托盘，免薰蒸，符合欧盟、北美各国对出口货物包装材料的法令要求；喷涂钢托盘适用于重载上货架之用，托盘表面根据需要制作成平板状、波纹状及间隔形式，满足不同的使用要求。