magmas的意思

magmas中文翻譯：

n.巖漿；熔巖；糊劑；乳漿劑（magma的復數）

相似詞語短語

starlings images───椋鳥圖片

magical story───神奇的故事

success magazine───成功雜志

bing images───必應bing圖像

image salon───形象沙龍

hog magazine───生豬雜志

magnetization resistance───磁化電阻

kmag yoyo───kmag yoyo

calaverite images───卡拉維特圖像

e-lander mags───e-lander彈夾

雙語使用場景

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，地質學家鮑溫和赫斯在地球上是否存在產生富含鎂的巖漿所需的高溫這一問題上存在分歧。

How does Etna produce its fiery mix of magmas?───埃特納如何制造出它炙熱的混合巖漿呢？

Normally, he said, volcanologists have to do "postmortem studies" of long-solidified magmas or study active lava.───的經驗，一般情況下，火山學家只能就凝結成巖的巖漿做一些“馬后炮”的工作，或者在火山噴發的時候以熔巖為研究材料。

Magmas in transit to the surface will further supplement this heat.───向地表運移的巖漿將進一步補充這種熱量。

Cinder cone volcanoes are formed when magmas with high gas contents and high viscosity are blown high into the air during an eruption.───火山渣錐火山是，當爆發時，高氣體含量和高粘度的熔巖被噴發到空氣中而形成的。

These magmas were then subjected to shallow level gabbroic fractionation, which led to larger chemical variation.───它們經受了淺層輝長巖質分離作用，化學變異較大。

Schiano and Clocchiatti are convinced that the similarity of the magmas is no coincidence.───希阿諾和克羅西亞提確信，這兩種巖漿的相似并非巧合。

Mafic dykes are believed to have derived from tholeiitic magmas under extension setting.───基性巖墻是伸展背景下，來自地幔的基性巖漿侵入體；

The petrogenesis of both the HT and LT magmas was further complicated by contamination of crust and lithospheric mantle.───HT和LT巖漿的巖石成因又進一步為地殼和巖石圈地幔的混染作用所復雜化。

英語使用場景

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.