magmas
美 [?mæɡm(xù)?]
英 ['mæɡm(xù)?] 
- n.(礦物,有機(jī)物等的)稀糊狀混合物;【地】巖漿;稠液;【藥】乳漿劑
詞形變化
復(fù)數(shù):magmata 復(fù)數(shù):magmas 同義詞
英漢解釋
n. | 1. (礦物,有機(jī)物等的)稀糊狀混合物;【地】巖漿;稠液;【藥】乳漿劑 |
英英解釋
例句
Magmas in transit to the surface will further supplement this heat.
向地表運(yùn)移的巖漿將進(jìn)一步補(bǔ)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(dāng)爆發(fā)時,高氣體含量和高粘度的熔巖被噴發(fā)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(jīng)受了淺層輝長巖質(zhì)分離作用,化學(xué)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(jìn)一步為地殼和巖石圈地幔的混染作用所復(fù)雜化。
Melt structure plays an important role in governing physical and thermodynamic characteristics of magmas .
熔體結(jié)構(gòu)對巖漿的物理和熱力學(xué)性質(zhì)起著重要的制約作用。
Long-term recycling of these materials will occur when they are melted to form magmas erupted from the Benioff zone.
當(dāng)這些物質(zhì)熔融形成巖漿,從貝尼奧夫帶噴發(fā)時,這些物質(zhì)將發(fā)生長期的再循環(huán)。
According to the chemical compositions, the 10 studied gabbros can be divided into two groups representing two different magmas.
10個輝長巖從化學(xué)組成上分為兩組,代表了兩個不同的巖漿。
Both island arc and mid-ocean ridge magmas apparently come from the mantle yet they have different compositions.
島弧和洋中脊火山巖都明顯來自地幔然而他們有不懂的組成。
Based on this, the petrologists pay more attentions to the origin of magmas instead to the evolution of granitic magmas.
基于此,巖石學(xué)家更注意花崗質(zhì)巖漿的起源而不是它們的演化。
New Constraints on the Origin and Evolution of Magmas and Fluids From the Crust and Upper Mantle;
地殼及上地幔巖漿和流體形成演化的新限制因素;