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1·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

2·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。

3·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。

4·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。

5·He said the widely accepted theory that when a volcano's magma chamber cools it could be years before it heats up with fresh magma could be wrong.

他声称，之前普遍为大众接受的理论可能是错的——即当火山岩浆库冷却后，需要经过多年才能在新岩浆的作用下重新恢复高温。

6·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.

第勒尼安海(Tyrrhenian Sea)是意大利以西地中海的一部分，马西里海山正位于第勒尼安海的海底，它有一个隐蔽但活跃的岩浆房。

7·The mechanism of this anti-order magmatic evolution is mainly caused by the separate crystallization of plagioclase in a high-level magma chamber.

这种反序岩浆演化的机制主要是由于斜长石在高位岩浆房中的分离结晶所致。

8·These factors include magma composition, convection, diffusion, thermal gradient, oxygen fugacity, temperature, pressure, the shape of magma chamber etc.

影响韵律形成的因素很多，通常包括岩浆成分、对流作用、扩散作用、热梯度、氧逸度、温度和压力等。

9·When the enormous magma chamber at Santorini finally collapsed to form the existing caldera, enormous tsunamis (tidal waves) spread outward in all directions.

圣多里尼火山的巨大岩浆房最后倒塌，形成了现有的喷火山口，巨大的海啸(潮汐波)向各个方面向外伸展。

10·The caldera is about 6.5 kilometers [4 miles] across. It formed following an eruption, when the emptied magma chamber collapsed under the weight of volcanic rock above it.

这座单体火山拥有几乎是世界上最大的完整火山喷口，这个直径约为6.5公里（4英里）的锅型火山口，是当熔岩从火山内腔流过时，上部的岩浆岩坍塌而形成的。