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首页> 外文期刊>Journal of Volcanology and Geothermal Research2012V243-244NOCT,15 >Video monitoring reveals pulsating vents and propagation path of fissure eruption during the March 2011 Pu'u 'O'o eruption, Kilauea volcano
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Video monitoring reveals pulsating vents and propagation path of fissure eruption during the March 2011 Pu'u 'O'o eruption, Kilauea volcano

机译:视频监控显示了2011年3月基拉韦厄火山Pu'u'O'o火山喷发期间脉动喷发孔和裂缝喷发传播路径

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摘要

Lava fountains are a common eruptive feature of basaltic volcanoes. Many lava fountains result from fissure eruptions and are associated with the alignment of active vents and rising gas bubbles in the conduit. Visual reports suggest that lava fountain pulses may occur in chorus at adjacent vents. The mechanisms behind such a chorus of lava fountains and the underlying processes are, however, not fully understood.
机译:熔岩喷泉是玄武岩火山的常见喷发特征。许多熔岩喷泉是裂隙喷发造成的,并且与主动喷口的对准和管道中上升的气泡有关。视觉报告表明,熔岩喷泉脉冲可能会出现在相邻通风口的合唱中。然而,这种熔岩喷泉合唱背后的机制和潜在的过程还没有被完全理解。

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