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首页> 外文期刊>Lithos: An International Journal of Mineralogy, Petrology, and Geochemistry >Metasomatic interaction of the eutectic Na- and K-bearing carbonate melts with natural garnet lherzolite at 6 GPa and 1100-1200 degrees C: Toward carbonatite melt composition in SCLM
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Metasomatic interaction of the eutectic Na- and K-bearing carbonate melts with natural garnet lherzolite at 6 GPa and 1100-1200 degrees C: Toward carbonatite melt composition in SCLM

机译:共晶Na-and碳酸盐碳酸盐在6GPa和1100-1200摄氏度下熔化的碳酸盐盐熔化的偏像相互作用:SCLM中的碳酸石熔融组合物

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摘要

The range of carbonatite melts in equilibrium with the subcontinental lithospheric mantle (SCLM) under geothermal conditions is limited by alkali-rich near-eutectic compositions. Therefore, here we employed eutectic Na/K-Ca-Mg-Fe carbonate mixtures to model the interaction of a metasomatic carbonatite melt with natural garnet lherzolite. The experiments were performed at 1100 and 1200 degrees C and 6 GPa in graphite capsules using a multianvil press. The run duration was 111 and 86 h, respectively. To verify achieving an equilibrium, a synthetic mixture identical to natural lherzolite was also employed.
机译:在地热条件下与亚平衡的亚型岩石罩(SCLM)熔化的碳酸石石熔化范围是受碱性近共晶组合物的限制。 因此,在这里,我们使用共晶Na / K-Ca-Mg-Fe碳酸盐混合物来模拟羟基碳酸盐熔体与天然石榴石芦荟的相互作用。 使用多聚体压机在石墨胶囊中以1100和1200℃和6GPa进行实验。 运行持续时间分别为111和86小时。 为了验证实现平衡,还采用了与天然甲绒石相同的合成混合物。

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