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Seismicity and outgassing dynamics of Nyiragongo volcano

机译:Nyiragongo火山的地震性和突出动态

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Active lava lakes at volcanoes can be regarded as open windows to their magmatic systems. The dynamics of such lakes may therefore provide decisive insights into deeper magmatic processes, potentially leading to fundamental theoretical implications and volcano monitoring improvements. Among the rare volcanoes on Earth hosting a persistent lava lake, Nyiragongo in D.R. Congo directly threatens a massive population of roughly 1 million inhabitants. Here we analyze close-range (i.e., summit) and distant (around 17 km) seismic measurements acquired at this African volcano between 2011 and 2018 in order to better understand the seismic signature of the lava lake activity and how it relates to the deeper volcanic processes. Both summit and distant seismic records contain a similar continuous tremor pattern attributable to the lava lake activity. Combining this information with time-lapse camera images and lava lake level measurements confirms the mechanism of gas pistoning at Nyiragongo, which is characterized by short-duration (a few minutes long) and meter-scale level variations during the period of observation. We also characterize the dominant periodicity of this shallow tremor signature of about a few tens of minutes. Because this marked periodic pattern varies during a significant one-month fluctuation of SO2 emissions (estimated from space), we suggest that this particular seismic periodicity corresponds to the convective lake movement driven by the persistent degassing typical of active open-vent volcanoes. Finally, new seismic evidence reveals the effect of deep magmatic intrusion and consequent major pressure changes in the plumbing system, resulting in sudden and large drops of the lava lake level associated with strong degassing. Such transient episodes have similar characteristics to total lava lake drainage associated with flank eruptions already observed at this volcano in 1977 and 2002, or at Kilauea volcano in 2018. (C) 2019 Elsevier B.V. All rights reser
机译:火山的活跃熔岩湖泊可被视为岩石系统的开窗。因此,这种湖泊的动态可以为更深的岩石过程提供决定性的洞察力,可能导致基本的理论意义和火山监测改进。在地球上的罕见火山中举办了一个持久的熔岩湖,Nyiragongo在D.R.刚果直接威胁着大约100万居民的大规模人口。在这里,我们在2011年和2018年间在这个非洲火山之间获得的近距离(即峰会)和遥远(约17公里)的地震测量,以便更好地了解熔岩湖活动的地震签名以及它与更深的火山有关的地震签名流程。峰会和遥远的地震记录均含有与熔岩湖活动的类似连续震颤模式。将此信息与时间流逝相机图像和熔岩湖级测量相结合,确认了Nyiragongo的气体清塞机制,其特征在于观察期间的短持续时间(几分钟长)和仪表级别变化。我们还表征了这个浅震颤签名的主导周期大约几十分钟。因为这种明显的周期性模式在SO2排放的显着的一个月波动(从空间估计)期间变化,所以建议这种特定地震周期性对应于由典型的活性开放式火山典型的持续脱气驱动的对流湖运动。最后,新的地震证据揭示了岩浆系统深层岩石侵入和随后​​的主要压力变化的影响,导致与强烈脱气相关的熔岩湖水平突然和大滴。这种瞬时事件必须与在这座火山在1977年和2002年,或在基拉韦厄火山2018年(C)2019爱思唯尔B.V.所有权利RESER已经观察到侧翼喷发相关的总熔岩湖排水类似的特征

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