首页> 外文期刊>Journal of Volcanology and Geothermal Research >The oscillation model of hydrothermal dynamics beneath Aso volcano, southwest Japan after small eruption on May 2011: A new understanding model using repeated absolute and relative gravity measurement
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The oscillation model of hydrothermal dynamics beneath Aso volcano, southwest Japan after small eruption on May 2011: A new understanding model using repeated absolute and relative gravity measurement

机译:2011年5月小喷发后日本西南部阿苏火山下面的热液动力学振荡模型:使用重复的绝对和相对重力测量的新理解模型

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摘要

At the end of 2010, the seismic activity in Aso volcano intensely increased and water level in the Nakadake crater decreased until early in 2011, then was followed by a small eruption in May 2011. After the eruption and heavy rain, the volcanic activity subsided to calm period, crater bottom was refilled with water, and water level increased in the Nakadake crater. The next tremor reappeared in 2014 and tracked to eruption in November 2014. This eruptive pattern and water level variation in the crater repeatedly appeared on the surface, and it should be related to the hydrothermal dynamics beneath Aso volcano.
机译:到2010年底,阿苏火山的地震活动急剧增加,中岳岳火山口的水位下降到2011年初,然后在2011年5月发生了一次小喷发。在喷发和大雨之后,火山活动消退了。平静时期,火山口底部重新注满水,Nakadake火山口的水位上升。下一次地震在2014年再次出现,并于2014年11月开始喷发。火山口的这种喷发模式和水位变化反复出现在地表,应该与阿苏火山下面的热液动力学有关。

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