Experimental Study of Chemical Counterdiffusion of Major Components (SiO2, Al2O3, Na2O, CaO, MgO, and FeO) and \({\text{CO}}_{3}^{{2 - }}\) Anion during Interaction of Basalt and Kimberlite Melts under Upper Mantle P–T Conditions

IF 1 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
E. S. Persikov, P. G. Bukhtiyarov, A. G. Sokol, A. N. Nekrasov, D. M. Sultanov
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引用次数: 0

Abstract

This paper reports new experimental results on the chemical counterdiffusion of major components (SiO2, Al2O3, Na2O, CaO, MgO, and FeO) and the \({\text{CO}}_{3}^{{2 - }}\) anion during interaction of basalt and kimberlite melts under upper-mantle pressure. The method of diffusion couples was employed on a BARS split-sphere apparatus at 5.5 GPa and 1850°C. It was shown that the rates of chemical counterdiffusion of all major melt species (SiO2, Al2O3, Na2O, CaO, MgO, and FeO) and the \({\text{CO}}_{3}^{{2 - }}\) anion are almost identical during interaction of model basalt and carbonate-bearing kimberlite melts and approximately an order of magnitude higher than the diffusion rates of these components during melt interaction under moderate pressures (100 MPa). The equal diffusion rates of CaO and \({\text{CO}}_{3}^{{2 - }}\) indicate that molecular CaCO3 diffusion from the kimberlitic to basaltic melt (model and natural) occurs also at the high pressure. The diffusion patterns are dramatically different during interaction of natural magnesian basalt and model kimberlite, which was observed for the interaction of these melts at moderate pressure. In addition to the molecular diffusion of CaCO3 into the magnesian basalt, the diffusion rates of other melt species increase significantly. All diffusing components show weak exponential dependence on concentrations approaching Di = const, similar to that observed during interaction of such melts at moderate pressures.

上地幔P-T条件下玄武岩-金伯利岩熔体相互作用中主要组分(SiO2、Al2O3、Na2O、CaO、MgO和FeO)和\({\text{CO}}_{3}^{{2 - }}\)阴离子的化学反扩散实验研究
本文报道了玄武岩与金伯利岩熔体在上地幔压力作用下,主要组分(SiO2、Al2O3、Na2O、CaO、MgO和FeO)和\({\text{CO}}_{3}^{{2 - }}\)阴离子的化学反扩散的新实验结果。在5.5 GPa和1850°C的BARS分裂球仪上采用扩散偶法。结果表明,模型玄武岩和含碳酸盐金伯利岩熔体相互作用过程中,所有主要熔体物质(SiO2、Al2O3、Na2O、CaO、MgO和FeO)和\({\text{CO}}_{3}^{{2 - }}\)阴离子的化学反扩散速率几乎相同,且在中等压力(100 MPa)下,其化学反扩散速率比这些成分在熔体相互作用过程中的扩散速率高一个数量级。CaO和\({\text{CO}}_{3}^{{2 - }}\)的扩散速率相等,表明CaCO3分子从金伯利岩向玄武岩熔体(模型熔体和天然熔体)扩散也发生在高压下。天然镁质玄武岩与模式金伯利岩在中压下相互作用时的扩散模式有显著差异。除CaCO3在镁质玄武岩中的分子扩散外,其他熔体物质的扩散速率均显著增加。所有扩散组分对接近Di = const的浓度表现出弱的指数依赖性,类似于在中等压力下这种熔体相互作用时观察到的情况。
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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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