首页> 外文期刊>Journal of Geological Research >Geochemistry of the Neoarchaean Volcanic Rocks of the Kilimafedha Greenstone Belt, Northeastern Tanzania
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Geochemistry of the Neoarchaean Volcanic Rocks of the Kilimafedha Greenstone Belt, Northeastern Tanzania

机译:坦桑尼亚东北部Kilimafedha绿岩带的新古生界火山岩的地球化学

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摘要

The Neoarchaean volcanic rocks of the Kilimafedha greenstone belt consist of three petrological types that are closely associated in space and time: the predominant intermediate volcanic rocks with intermediate calc-alkaline to tholeiitic affinities, the volumetrically minor tholeiitic basalts, and rhyolites. The tholeiitic basalts are characterized by slightly depleted LREE to nearly flat REE patterns with no Eu anomalies but have negative anomalies of Nb. The intermediate volcanic rocks exhibit very coherent, fractionated REE patterns, slightly negative to absent Eu anomalies, depletion in Nb, Ta, and Ti in multielement spidergrams, and enrichment of HFSE relative to MORB. Compared to the other two suites, the rhyolites are characterized by low concentrations of TiO_2 and overall low abundances of total REE, as well as large negative Ti, Sr, and Eu anomalies. The three suites have a εNd (2.7 Ga) values in the range of ?0.51 to +5.17. The geochemical features of the tholeiitic basalts are interpreted in terms of derivation from higher degrees of partial melting of a peridotite mantle wedge that has been variably metasomatized by aqueous fluids derived from dehydration of the subducting slab. The rocks showing intermediate affinities are interpreted to have been formed as differentiates of a primary magma formed later by lower degrees of partial melting of a garnet free mantle wedge that was strongly metasomatized by both fluid and melt derived from the subducting oceanic slab. The rhyolites are best interpreted as having been formed by shallow level fractional crystallization of the intermediate volcanic rocks involving plagioclase and Tirich phases like ilmenite and magnetite as well as REE-rich phases like apatite, zircon, monazite, and allanite. The close spatial association of the three petrological types in the Kilimafedha greenstone belt is interpreted as reflecting their formation in an evolving late Archaean island arc.
机译:Kilimafedha绿岩带的新古宙火山岩由三种在空间和时间上密切相关的岩石学类型组成:主要的中火山岩与钙对碱的亲和力与钙钛矿的亲和力中等,体积较小的辉石玄武岩和流纹岩。孔雀状玄武岩的特征是,LREE略微耗尽至接近平坦的REE模式,没有Eu异常,但是Nb呈负异常。中火山岩表现出非常连贯的,分馏的REE模式,对不存在Eu异常略有负面影响,多元素蜘蛛图中Nb,Ta和Ti的耗竭,以及相对于MORB的HFSE富集。与其他两个套件相比,流纹岩的特征在于TiO_2的浓度低,总REE的总体丰度低,以及较大的负Ti,Sr和Eu异常。这三个套件的εNd(2.7 Ga)值在〜0.51至+5.17的范围内。高渗玄武岩的地球化学特征是根据橄榄岩地幔楔的部分熔融程度较高而解释的,而橄榄岩幔楔的高度融化作用是由俯冲板脱水产生的含水流体变质作用的。表现出中等亲和力的岩石被解释为后来形成的初级岩浆的差异,该初级岩浆是通过低石榴石游离地幔楔的部分融化程度而形成的,该楔融被俯冲的大洋板块中的流体和熔体强烈地交化了。流纹岩最好被解释为是由中间火山岩的浅层分级结晶形成的,该中间火山岩包括斜长石和Tirich相(如钛铁矿和磁铁矿)以及富含REE的相(磷灰石,锆石,独居石和尿囊石)。 Kilimafedha绿岩带中三种岩石学类型的紧密空间联系被解释为反映了它们在不断演变的太古宙岛弧中的形成。

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