magmas发音

意思翻译

n.岩浆；熔岩；糊剂；乳浆剂（magma的复数）

相似词语短语

starlings images───椋鸟图片

magical story───神奇的故事

success magazine───成功杂志

bing images───必应bing图像

image salon───形象沙龙

hog magazine───生猪杂志

magnetization resistance───磁化电阻

kmag yoyo───kmag yoyo

calaverite images───卡拉维特图像

e-lander mags───e-lander弹夹

双语使用场景

Prior to 1960, geologists Bowen and Hess disagreed over whether or not the very high temperatures needed to produce magmas rich in magnesium could have existed on Earth.───之前，地质学家鲍温和赫斯在地球上是否存在产生富含镁的岩浆所需的高温这一问题上存在分歧。

How does Etna produce its fiery mix of magmas?───埃特纳如何制造出它炙热的混合岩浆呢？

Normally, he said, volcanologists have to do "postmortem studies" of long-solidified magmas or study active lava.───的经验，一般情况下，火山学家只能就凝结成岩的岩浆做一些“马后炮”的工作，或者在火山喷发的时候以熔岩为研究材料。

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。

Cinder cone volcanoes are formed when magmas with high gas contents and high viscosity are blown high into the air during an eruption.───火山渣锥火山是，当爆发时，高气体含量和高粘度的熔岩被喷发到空气中而形成的。

These magmas were then subjected to shallow level gabbroic fractionation, which led to larger chemical variation.───它们经受了浅层辉长岩质分离作用，化学变异较大。

Schiano and Clocchiatti are convinced that the similarity of the magmas is no coincidence.───希阿诺和克罗西亚提确信，这两种岩浆的相似并非巧合。

Mafic dykes are believed to have derived from tholeiitic magmas under extension setting.───基性岩墙是伸展背景下，来自地幔的基性岩浆侵入体；

The petrogenesis of both the HT and LT magmas was further complicated by contamination of crust and lithospheric mantle.───HT和LT岩浆的岩石成因又进一步为地壳和岩石圈地幔的混染作用所复杂化。

英语使用场景

Not all magmas have the same composition, and magmas with different compositions melt at different temperatures.

Isotopic compositions of continental intraplate mantle-derived magmas commonly vary as a function of lithospheric age.

The contrast between gas-rich and gas-poor magmas is much more pronounced at the viscous granitic end of the scale.

These magmas were then subjected to shallow level gabbroic fractionation, which led to larger chemical variation.

One possibility is thatthetwo magmas form at different locations and mix somewhere within Etna 's plumbing system.

In fluid magmas, such as those of basaltic composition, these gas bubbles can expand freely.

Perhaps there are no lamprophyre magmas, and lamprophyres derive from common basic magmas which are contaminated by the crust in their source or the process of emplacement.

Magmas erupted at mid-ocean ridges are derived from the upper mantle.

Comparison of their chemistry with that of magmas erupted on oceanic islands demonstrates the plumes differ chemically from the upper mantle.