magmas

magmas的基本解释

n.

岩浆( magma的名词复数 )

与magmas相关的网络例句 [注：此内容来源于网络，仅供参考]

So, the density of primary basaltic magmas is a important criteria to distinguish geodynamics settings in which magmas formed.

原生岩浆密度可作为判定岩浆产出的地球动力学背景的重要标志之一。

Based on this, the petrologists pay more attentions to the origin of magmas instead to the evolution of granitic magmas.

基于此，岩石学家更注意花岗质岩浆的起源而不是它们的演化。

The collision and orogenesis, the intrusion of magmas and the formation of ore deposits were occurred sequentially.

两者在时间上的连续性，进一步说明了成矿作用与构造时间的耦合，碰撞造山-岩浆侵位-矿床的形成是一统一的连续过程。

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。

Its volcanic geological formation is complicated, varying from hard lava magmas to weathering pyroclastic debris.

火山形成的地层非常复杂，从坚硬的火山熔岩到松软风化的火山碎屑堆积物都有存在。

与magmas相关的网络解释 [注：此内容来源于网络，仅供参考]

Martian magmas：火星

martensitic-type phase transformation ==> 马氏体式相变化 | Martian magmas ==> 火星のマグマ | Martin Heidegger ==> 马丁.海德格尔=>マルティン?ハイデッガー

segregation in magmas：岩浆分体作用;岩浆分凝作用

岩浆分结作用;岩浆分凝 magmatic segregation | 岩浆分体作用;岩浆分凝作用 segregation in magmas | 岩浆分体作用;岩浆分凝作用 magmatic segregation