magma chamber信息详情
[地物]岩浆房；岩浆库；岩浆储源
magma───n.[地质]岩浆；糊剂；n.(Magma)人名；(英)马格马
chamber───n.(Chamber)人名；(英)钱伯；n.（身体或器官内的）室，膛；房间；会所；adj.室内的；私人的，秘密的；vt.把…关在室内；装填（弹药等）
silicic magma───硅质岩浆
council chamber───n.会议室
gas chamber───n.毒气室
cooled magma───冷却岩浆
phonolite magma───响岩岩浆
basaltic magma───[地质]玄武岩浆
air chamber───n.气囊，气胞; 气室
As the land above the magma chamber collapses, immense gray clouds called pyroclastic flows burst out horizontally all around the caldera.───当岩浆库上方的陆地崩陷，称为火山碎屑流的巨大灰色云雾，会突然由火山臼的周围向外水平散开。
Related news: "Vesuvius Magma Chamber Rising; May Mean Milder Eruption" [September 10, 2008].───相关新闻：“ 维苏威火山岩浆房上升，或许将会有较缓和的喷发”，2008年9月10日
However, the temperatures and oxygen fugacity of magmas at high level magma chamber decreased along with fractional crystallization.───但在高位岩浆房中，随着分离结晶作用的进行，岩浆的温度和氧逸度逐渐降低。
If this model works, and you can rejuvenate a magma chamber by a pulse of magma, you can kick off an eruption when you weren't expecting it.───“如果这个模型正确的话，那么我们就能通过一个脉冲的岩浆再度激活岩浆库，也可以阻止没有预料到的喷发”。
Notably, as researchers soon realized, not every large magma chamber will necessarily erupt catastrophically.───尤其是当研究人员很快发现，并不是每个大型岩浆库都一定会造成灾难性爆发。
Magma chamber at the base of continental crust and within the crust may control the development of systems and subsystems, respectively.───壳底岩浆房和壳内岩浆房分别控制系统和亚系统的形成及其分布。
Related news: "Vesuvius Magma Chamber Rising; May Mean Milder Eruption" [September 10, 2008].───相关新闻：“维苏威火山岩浆房上升，或许将会有较缓和的喷发”，2008年9月10日
They were not above a magma chamber.───它们不在岩浆房上面。
Likewise, a reheated magma chamber doesn't always lead to an eruption, the study authors noted.───同样的，一个再度受热的岩浆库并非总是导致喷发，研究作者指出。
We envisage a convecting magma chamber of height H, cooled from above.
Marsili has a hidden but active magma chamber and lies beneath the surface of the Tyrrhenian Sea, which is part of the Mediterranean west of Italy.
These factors include magma composition, convection, diffusion, thermal gradient, oxygen fugacity, temperature, pressure, the shape of magma chamber etc.
Instead it slowly froze in a magma chamber into a mush of coarse crystals.
However, the temperatures and oxygen fugacity of magmas at high level magma chamber decreased along with fractional crystallization.
The mechanism allows for great variation and complexity in magma chamber sedimentation.