Silicate melt inclusions in ignimbrites, Bükkalja Volcanic Field, Northern Hungary - texture and geochemistry

R. Lukács, G. Czuppon, S. Harangi, C. Szabó, T. Ntaflos, F. Koller
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引用次数: 12

Abstract

Silicate melt inclusions are frequent in the phenocryst phases (quartz, plagioclase, orthopyroxene, ilmenite and accessory minerals) of the Miocene silicic pyroclastic rocks of the Bukkalja Volcanic Field, Northern Hungary. These melt inclusions were trapped at different stages of magma evolution; therefore, they provide important information on the petrogenetic processes. The melt inclusions in the Bukkalja pyroclastic rocks show various textures such as (1) wholly enclosed type; (2) hourglass inclusions and (3) reentrant or embayment glass. Among the wholly enclosed type melt inclusions further textural subgroups can be distinguished based on their shape: negative crystal, rounded, elongated and irregular shaped. These various textures reflect differences in the time of entrapment prior to eruption and in the post-entrapment condition in the magma chamber. The largest textural variation was found in the quartz-hosted melt inclusions. However, the major element compositions of these melt inclusions do no...
匈牙利北部b kkalja火山带火成岩中的硅酸盐熔体包裹体——结构与地球化学
匈牙利北部Bukkalja火山田中新世硅质火山碎屑岩的斑晶相(石英、斜长石、正辉石、钛铁矿及其附属矿物)中常见硅酸盐熔体包裹体。这些熔融包裹体是在岩浆演化的不同阶段被圈闭的;因此,它们提供了岩石形成过程的重要信息。Bukkalja火山碎屑岩中的熔体包裹体具有多种结构,如:(1)全封闭型;(2)沙漏夹杂物和(3)可重入或镶嵌玻璃。在全封闭型熔体包裹体中,根据其形状可划分出负晶型、圆形、细长型和不规则型等结构亚群。这些不同的结构反映了岩浆房内喷发前圈闭时间和圈闭后条件的差异。石英熔融包裹体的结构变化最大。然而,这些熔体包裹体的主要元素组成并没有…
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