Tremor di Gunungapi Raung

V. L. Ipmawan
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Abstract

Crisis period of Raung Volcano, located in East of Java, Indonesia, was started in November 2014. The seismicity of Raung Volcano was dominated by volcanic tremor. Volcanic tremor can be related with internal process of a volcano and can be a fruitful tool to understand the physical process inside the volcano. The intensity of tremor event in early crisis period is low but increases quickly then followed by the continuous tremor in the next month, December 2014. The dominant frequency of Raung volcano has range 1 ± 0,2 Hz. We suggest that there are two resonators exciting tremor signal based on the number of peaks in Raung’s tremor spectrum.
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2014年11月,位于印尼爪哇岛东部的朗火山进入危机时期。琅火山地震活动以火山震颤为主。火山震颤与火山内部活动有关,是了解火山内部物理活动的有效工具。危机初期震颤事件强度较低,但迅速增加,随后在2014年12月连续发生震颤。琅火山的主导频率范围为1±0.2 Hz。根据朗氏震颤谱的峰数,我们认为有两个谐振器激励震颤信号。
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