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- W2050180242 abstract "An experimental method for directly determining the degree of interconnectivity of melt in a partially molten system is discussed using an olivine-basalt system as an example. Samarium 151 is allowed time to diffuse through mixtures of olivine and basalt powder which have texturally equilibrated at 1350°C and 13 to 15 kbars. The final distribution of samarium is determined through examination of developed radiographs of the samples. A uniform distribution of samarium throughout an entire sample implies that melt is present as an interconnected network because diffusion of samarium along melt-free grain boundaries is shown not to occur in the time frame of these experiments. Quantitative determination of the degree of interconnectivity is done by establishing a one to one correspondence between a sample and its radiograph. Results suggest an interconnected melt network is established at melt fractions at least as low as 1 wt % and all melt is completely interconnected at melt fractions at least as low as 2 wt % for the system examined." @default.
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- W2050180242 date "1988-12-01" @default.
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- W2050180242 title "An experimental method for directly determining the interconnectivity of melt in a partially molten system" @default.
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- W2050180242 doi "https://doi.org/10.1029/gl015i013p01459" @default.
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