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东非裂谷Oldoinyo Lengai火山碳酸岩浆作用过程中的镁同位素分馏
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摘要
<正>碳酸盐熔体具有极低的粘度和独特的元素配分型式,是引起地幔交代作用和化学组成不均一性的重要介质之一(Yaxley et al.,1991;Rudnick et al.,1993;Coltorti et al.,1999)。火成碳酸岩是碳酸盐熔体结晶的产物,其镁(Mg)同位素组成可以为碳酸岩浆作用过程中镁同位素的分馏行为和地幔的镁同位素组成特征提供重要制约。为此,我们系统研究了东非裂谷Oldoinyo Lengai火山共生的火成碳
引文
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    Teng Fangzhen,Li Wangye,Ke Shan,Marty B,Dauphas N,Huang Shichun,Wu Fuyuan,Pourmand A.2010.Magnesium isotopic composition of the Earth and chondrites.Geochimica et Cosmochimica Acta,74(14):4150~4166.
    Xiao Yan,Teng Fangzhen,Zhang Hongfu,Yang Wei.2013.Large magnesium isotope fractionation in peridotite xenoliths from eastern North China craton:Product of melt-rock interaction.Geochimica et Cosmochimica Acta,115:241~261.
    Yang Wei,Teng Fangzhen,Zhang Hongfu.2009.Chondritic magnesium isotopic composition of the terrestrial mantle:A case study of peridotite xenoliths from the North China craton.Earth and Planetary science Letters,288(3-4):475~482.
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