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首页> 外文期刊>Journal of Volcanology and Geothermal Research >Magmatic plumbing systems of the monogenetic volcanic fields: A case study of Tolbachinsky Dol, Kamchatka
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Magmatic plumbing systems of the monogenetic volcanic fields: A case study of Tolbachinsky Dol, Kamchatka

机译:单相火山岩岩浆管道系统:以堪察加半岛的托尔巴金斯基山为例

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Clusters of small-volume volcanoes that individually may be defined as monogenetic, but have interlinked and interconnected plumbing systems, are used to be categorized as monogenetic volcanic fields (MVF). We argue that such volcanic clusters should be distinguished as separate type of volcanism, intermediate between monogenetic and polygenetic. The magma plumbing system structure of the MVF (its complexity and polymagmatic character) is the key argument for the potential separation of them in a classification. To avoid confusion caused by genetic meaning of the used words we suggest using a term "areal volcanism" or "areal volcanic fields" (AVF instead of MVF) as defining this special type of volcanic activity. Here we provide a review of the main characteristic features of one of the largest Holocene AVF, which is active now - the Tolbachik field of cinder cones in the southern part of Klyuchevskaya volcano group (Kamchatka), known in the literature as Tolbachinsky Dol. This paper is focused on the research of magma plumbing system. We consider structural, morphological, geological, geochemical and petrological data on the erupted basalts and their genesis. Specially planned seismic experiments made in 2010-2015 (seismic tomography and microseismic sounding) allowed modeling of the principal elements of the magma plumbing system of Tolbachik AVF. Analysis of the investigations made in this area shows that Tolbachik AVF has a complex, dynamic, variable magmatic feeding system, which can be visualized as a superposition of subvertical and sublateral magma conduits. The contrast composition of the erupted rocks is caused by their different, although genetically connected, magma sources and mixing processes. One of the long-lived eruptive centers of Tolbachik AVF is Plosky Tolbachik stratovolcano, which lost its independent activity and was captured by Tolbachik AVF in Holocene. The AVF formed rejuvenated volcanism using the feeding system of the stratovolcano like an "old anthill". The magma plumbing system characteristics of Tolbachinsky Dol strongly support the idea of separation of AVF from monogenetic volcanism type in the classification. (C) 2018 Elsevier B.V. All rights reserved.
机译:小体积火山群可单独定义为单基因火山群,但具有相互连接和互连的管道系统,通常被归类为单基因火山场(MVF)。我们认为,此类火山岩团应区分为单独的火山作用类型,介于单基因和多基因之间。 MVF的岩浆管道系统结构(其复杂性和多岩浆特征)是在分类中潜在分离它们的关键论点。为避免因所用单词的遗传含义引起的混淆,我们建议使用术语“区域火山活动”或“区域火山场”(AVF代替MVF)来定义这种特殊类型的火山活动。在这里,我们对最大的全新世AVF的主要特征进行了综述,该活动目前正在活跃-Klyuchevskaya火山群(Kamchatka)南部的煤渣锥的Tolbachik场,在文献中称为Tolbachinsky Dol。本文的重点是岩浆管道系统的研究。我们考虑了玄武岩喷发及其成因的结构,形态,地质,地球化学和岩石学数据。在2010-2015年进行的特别计划的地震实验(地震层析成像和微震探测)允许对Tolbachik AVF岩浆管道系统的主要要素进行建模。对这方面研究的分析表明,托尔巴奇克AVF有一个复杂的,动态的,可变的岩浆进给系统,可以将其可视化为垂直和副岩浆导管的叠加。喷发岩石的反差成分是由它们虽然具有遗传联系的岩浆源和混合过程不同而引起的。 Tolbachik AVF的长寿喷发中心之一是Plosky Tolbachik Stratovolcano,它失去了独立的活动,并被Tolbachik AVF在全新世捕获。 AVF使用层状火山的进给系统像“老蚁丘”一样形成了复兴的火山。 Tolbachinsky Dol的岩浆管道系统特征强烈支持在分类中将AVF与单基因火山类型分离的想法。 (C)2018 Elsevier B.V.保留所有权利。

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