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Seismic detection of increased degassing before Kīlauea's 2008 summit explosion

机译:在基拉韦厄(Kīlauea)2008年峰会爆炸之前,通过地震检测发现脱气加剧

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The 2008 explosion that started a new eruption at the summit of Kīlauea Volcano, Hawai‘i, was not preceded by a dramatic increase in earthquakes nor inflation, but was associated with increases in SO2 emissions and seismic tremor. Here we perform shear wave splitting analysis on local earthquakes spanning the onset of the eruption. Shear wave splitting measures seismic anisotropy and is traditionally used to infer changes in crustal stress over time. We show that shear wave splitting may also vary due to changes in volcanic degassing. The orientation of fast shear waves at Kīlauea is usually controlled by structure, but in 2008 showed changes with increased SO2 emissions preceding the start of the summit eruption. This interpretation for changing anisotropy is supported by corresponding decreases in V p/ V s ratio. Our result demonstrates a novel method for detecting changes in gas flux using seismic observations and provides a new tool for monitoring under-instrumented volcanoes.
机译:2008年的爆炸在夏威夷基拉韦厄火山的山顶上开始了新的喷发,而地震和通货膨胀却没有急剧增加,但与SO 2 排放量和地震震颤相关。在这里,我们对爆发期间发生的局部地震进行了剪切波分裂分析。剪切波分裂测量地震各向异性,并且传统上用来推断地壳应力随时间的变化。我们表明,剪切波分裂也可能由于火山脱气的变化而变化。基拉韦厄的快速切变波的方向通常受结构控制,但在2008年峰顶爆发前,SO 2 排放增加,表明变化。 V p / V s 比值的相应降低支持这种改变各向异性的解释。我们的结果证明了一种使用地震观测值检测气体通量变化的新方法,并提供了一种监测仪器不足的火山的新工具。

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