青年中文magma chamber的意思
magma chamber中文翻譯：
[地物]巖漿房；巖漿庫；巖漿儲源
magma───n.[地質]巖漿；糊劑；n.(Magma)人名；(英)馬格馬
chamber───n.(Chamber)人名；(英)錢伯；n.（身體或器官內的）室，膛；房間；會所；adj.室內的；私人的，秘密的；vt.把…關在室內；裝填（彈藥等）
silicic magma───硅質巖漿
council chamber───n.會議室
gas chamber───n.毒氣室
cooled magma───冷卻巖漿
phonolite magma───響巖巖漿
basaltic magma───[地質]玄武巖漿
air chamber───n.氣囊，氣胞; 氣室
As the land above the magma chamber collapses, immense gray clouds called pyroclastic flows burst out horizontally all around the caldera.───當巖漿庫上方的陸地崩陷，稱為火山碎屑流的巨大灰色云霧，會突然由火山臼的周圍向外水平散開。
Related news: "Vesuvius Magma Chamber Rising; May Mean Milder Eruption" [September 10, 2008].───相關新聞：“ 維蘇威火山巖漿房上升，或許將會有較緩和的噴發”，2008年9月10日
However, the temperatures and oxygen fugacity of magmas at high level magma chamber decreased along with fractional crystallization.───但在高位巖漿房中，隨著分離結晶作用的進行，巖漿的溫度和氧逸度逐漸降低。
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.───“如果這個模型正確的話，那么我們就能通過一個脈沖的巖漿再度激活巖漿庫，也可以阻止沒有預料到的噴發”。
Notably, as researchers soon realized, not every large magma chamber will necessarily erupt catastrophically.───尤其是當研究人員很快發現，并不是每個大型巖漿庫都一定會造成災難性爆發。
Magma chamber at the base of continental crust and within the crust may control the development of systems and subsystems, respectively.───殼底巖漿房和殼內巖漿房分別控制系統和亞系統的形成及其分布。
Related news: "Vesuvius Magma Chamber Rising; May Mean Milder Eruption" [September 10, 2008].───相關新聞：“維蘇威火山巖漿房上升，或許將會有較緩和的噴發”，2008年9月10日
They were not above a magma chamber.───它們不在巖漿房上面。
Likewise, a reheated magma chamber doesn't always lead to an eruption, the study authors noted.───同樣的，一個再度受熱的巖漿庫并非總是導致噴發，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.