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首页> 外文期刊>Contributions to Mineralogy and Petrology >Formation of cordierite-bearing lavas during anatexis in the lower crust beneath Lipari Island (Aeolian arc, Italy)
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Formation of cordierite-bearing lavas during anatexis in the lower crust beneath Lipari Island (Aeolian arc, Italy)

机译:利帕里岛(意大利风弧)下下部地壳中的食蚁兽在食盐期形成堇青石熔岩。

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Cordierite-bearing lavas (CBL; ~ 105 ka) erupted from the Mt. S. Angelo volcano at Lipari (Aeolian arc, Italy) are high-K andesites, displaying a range in the geochemical and isotopic compositions that reflect heterogeneity in the source and/or processes. CBL consist of megacrysts of Ca-plagioclase and clinopyroxene, euhedral crystals of cordierite and garnet, microphenocrysts of orthopyroxene and plagioclase, set in a heterogeneous rhyodacitic-rhyolitic groundmass containing abundant metamorphic and gabbroic xenoliths. New petrographic, chemical and isotopic data indicate formation of CBL by mixing of basaltic-andesitic magmas and high-K peralu-minous rhyolitic magmas of anatectic origin and characterize partial melting processes in the lower continental crust of Lipari. Crustal anatectic melts generated through two main dehydration-melting peritectic reactions of metasedimentary rocks: (1) Biotile -f- Aluminosilicate + Quartz + Albite = Garnet + Cordierite + K-feldspar + Me (2) Biotite + Garnet + Quartz = Orthopyroxene + Cordierite + K-feldspar + Melt. Their position into the petrogenetic grid suggests that heating and consequent melting of metasedimentary rocks occurred at temperatures of 725
机译:山上喷出了含堇青石的熔岩(CBL;〜105 ka)。 Lipari(意大利风神弧)的S. Angelo火山是高钾安山岩,在地球化学和同位素组成方面显示出一定范围,可反映出源和/或过程的非均质性。 CBL由Ca-斜长石和斜生辉石的大晶体,堇青石和石榴石的自体晶体组成,邻苯二酚和斜长石的微细晶石组成,位于含有丰富的变质和辉长岩异种岩的非均质的流纹岩-流纹岩地层中。新的岩石学,化学和同位素数据表明,玄武质安山岩和安第斯高钾钾流纹岩浆岩混合形成了CBL,并表征了利帕里下部陆壳的部分熔融过程。沉积物岩石的两个主要的脱水熔融包晶反应产生了地壳的阳极熔体:(1)生物质-f-铝硅酸盐+石英+阿尔比特=石榴石+堇青石+钾长石+熔体; (2)黑云母+石榴石+石英=邻辉石+堇青石+钾长石+熔体。它们在成岩网格中的位置表明,变质沉积岩的加热和随后的融化发生在725

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