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首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >Dynamic plumbing system beneath volcanoes revealed by kinetic modeling, and the connection to monitoring data: An example from Mt. Etna
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Dynamic plumbing system beneath volcanoes revealed by kinetic modeling, and the connection to monitoring data: An example from Mt. Etna

机译:动力学建模揭示了火山下面的动态管道系统,并与监测数据建立了联系:埃特纳火山

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Our ability to monitor volcanoes (using seismic signals, ground deformation, gas fluxes, or other ground and satellite based observations) as well as our understanding of melt reservoirs that feed eruptions have evolved tremendously in recent years. The complex plumbing systems that are thought to feed eruptions are, however, difficult to relate to the monitoring signals. Here we show that the record preserved in compositional zoning of erupted minerals may be used to reconstruct sections of the plumbing system. Kinetic modeling of such zoning can yield information on the residence time of magma in different segments of the plumbing systems. This allows a more nuanced evaluation of the link between observed monitoring signals or eruption styles and the magmatic processes and movement of batches of melts at depth. The approach is illustrated through a study of the compositional zoning recorded in olivine crystals from the 1991-1993 SE-flank eruption products of Mt. Etna (Sicily). The zoning patterns in crystals reveal that the plumbing system of the volcano consisted of at least three different magmatic environments between which magma was transported and mixed in the year or two preceding the start of eruption. Quantification of this history indicates that two main pathways of melt migration and three timescales dominated the dynamics of the system. Combination of this information with the timing of observation of various monitoring signals allows a reconstruction of the dynamic evolution of this section of the plumbing system during the early stages of the 1991-1993 eruption. It is seen, for example, how the migration of melt through the same sections of the plumbing system can cause pre-eruptive triggering, enhance Strombolian activity, and through the ensuing eruption cleanse and flush the plumbing system. Different kinds of mixing occur simultaneously at different sections of the plumbing system on different timescales (a few days up to two years).
机译:近年来,我们监测火山的能力(使用地震信号,地面变形,气体通量或其他基于地面和卫星的观测结果)以及对馈入喷发的熔体储层的了解已发生了巨大变化。但是,复杂的管道系统被认为是喷发的,很难与监测信号联系起来。在这里,我们表明,保留在喷发矿物成分分区中的记录可用于重建管道系统的各个部分。这种分区的动力学模型可以产生关于岩浆在管道系统的不同部分中的停留时间的信息。这样可以对观察到的监测信号或喷发类型与岩浆过程和深处熔体批次之间的联系进行更细致的评估。通过对1991-1993年Mt山脉SE侧面喷发产物橄榄石晶体中记录的成分分区进行的研究来说明这种方法。埃特纳火山(西西里岛)。晶体中的分区模式表明,火山的管道系统由至少三种不同的岩浆环境组成,在喷发开始前的一两年内,岩浆在其中被运输和混合。对该历史的量化表明,熔体迁移的两个主要途径和三个时标主导了系统的动力学。将此信息与各种监视信号的观测时间相结合,可以重建1991-1993年喷发早期该管道系统这一部分的动态演变。例如,可以看到熔体通过管道系统相同部分的迁移如何引起喷发前的触发作用,增强Strombolian的活动,并通过随后的喷发清洁和冲洗管道系统。不同类型的混合同时发生在管道系统的不同部分,时间跨度不同(几天到两年不等)。

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