梅杰日亚火山口镁质玄武岩:优势岩浆及其来源——以千岛群岛伊图鲁普岛Menshiy Brat火山为例

IF 1 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
D. V. Kuzmin, I. R. Nizametdinov, S. Z. Smirnov, T. Yu. Timina, A. Ya. Shevko, M. P. Gora, A. V. Rybin
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引用次数: 0

摘要

本文介绍了伊图鲁普岛Medvezhia火山口Menshiy Brat火山口后火山玄武岩形成条件的新资料。液态矿物组合由橄榄石(Fo = 85.3 ~ 90.1 mol %)和铬尖晶石(Cr = 0.46 ~ 0.6)组成,在喷发过程中结晶温度为1090 ~ 1170℃,氧逸度为NNO + 0.6 (σ = 0.2) ~ NNO + 0.2 (σ = 0.14)。液相橄榄石熔体包裹体数据表明,其母熔体为低al2o3和低k2o, MgO含量高达15.5 wt %,平均H2O含量为5.5 wt %。新获得的含橄榄石熔体包裹体挥发性含量数据表明,基性熔体是在板岩衍生流体的积极影响下,由富含橄榄岩的源与少量不含橄榄石成分的混合物在1225°C下部分熔融而产生的。这些流体是从俯冲板块中分离出来的,温度为670-705°C,深度为Iturup岛下方95-105公里。我们的研究结果增强了我们对基性岩浆演化的理解,这些岩浆在大型火山口形成过程中作为热量和挥发源。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Magnesian Basalts of the Medvezhia Caldera: Dominant Magmas and Their Sources, as Exemplified by Menshiy Brat Volcano, Iturup Island, Kuriles

Magnesian Basalts of the Medvezhia Caldera: Dominant Magmas and Their Sources, as Exemplified by Menshiy Brat Volcano, Iturup Island, Kuriles

The paper presents new data on the formation conditions of basalts from Menshiy Brat postcaldera volcano in the Medvezhia caldera, Iturup Island. The liquidus mineral assemblage consists of olivine (Fo 85.3–90.1 mol %) and chromium spinel (Cr# = 0.46–0.6), which crystallized at 1090–1170°C and oxygen fugacity at NNO + 0.6 (σ = 0.2) to NNO + 0.2 (σ = 0.14) in the course of the eruption. Data on melt inclusions in the liquidus olivine demonstrate that its parental melts were low-Al2O3 and low-K2O, with up to 15.5 wt % MgO, and with an average H2O content of 5.5 wt %. The newly obtained data on volatile contents in the olivine-hosted melt inclusions suggest that the mafic melts were derived by the partial melting of a peridotitic-rich source with a small admixture of an olivine-free component at 1225°C, under active influence of the slab-derived fluids. These fluids were separated from the subducting slab at 670–705°C and depths of 95–105 km beneath Iturup Island. Our results enhance our understanding of the evolution of basic magmas that serve as a heat and volatile sources during the formation of large calderas.

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来源期刊
Petrology
Petrology 地学-地球科学综合
CiteScore
2.40
自引率
20.00%
发文量
27
审稿时长
>12 weeks
期刊介绍: Petrology is a journal of magmatic, metamorphic, and experimental petrology, mineralogy, and geochemistry. The journal offers comprehensive information on all multidisciplinary aspects of theoretical, experimental, and applied petrology. By giving special consideration to studies on the petrography of different regions of the former Soviet Union, Petrology provides readers with a unique opportunity to refine their understanding of the geology of the vast territory of the Eurasian continent. The journal welcomes manuscripts from all countries in the English or Russian language.
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