Electrical conductivity of basaltic and carbonatite melt-bearing peridotites at high pressures: Implications for melt distribution and melt fraction in the upper mantle

• Published in: Earth and planetary science letters 2010-07, Vol.295 (3), p.593-602
• Main Authors: Yoshino, Takashi, Laumonier, Mickael, McIsaac, Elizabeth, Katsura, Tomoo
• Format: Article
• Language: English
• Subjects: basalt; Carbonates; carbonatite; Earth Sciences; electrical conductivity; Electrical resistivity; Environmental Sciences; Global Changes; Mantle; Mathematical models; melt fraction; Melts; Olivine; permeability; Resistivity; Sciences of the Universe; Silicates; Stress concentration; Volcanology
• ISSN: 0012-821X; 1385-013X
• DOI: 10.1016/j.epsl.2010.04.050

Electrical impedance measurements were performed on two types of partial molten samples with basaltic and carbonatitic melts in a Kawai-type multi-anvil apparatus in order to investigate melt fraction–conductivity relationships and melt distribution of the partial molten mantle peridotite under high pressure. The silicate samples were composed of San Carlos olivine with various amounts of mid-ocean ridge basalt (MORB), and the carbonate samples were a mixture of San Carlos olivine with various amounts of carbonatite. High-pressure experiments on the silicate and carbonate systems were performed up to 1600 K at 1.5 GPa and up to at least 1650 K at 3 GPa, respectively. The sample conductivity increased with increasing melt fraction. Carbonatite-bearing samples show approximately one order of magnitude higher conductivity than basalt-bearing ones at the similar melt fraction. A linear relationship between log conductivity ( σ bulk) and log melt fraction ( ϕ) can be expressed well by the Archie's law (Archie, 1942) ( σ bulk/ σ melt = Cϕ n ) with parameters C = 0.68 and 0.97, n = 0.87 and 1.13 for silicate and carbonate systems, respectively. Comparison of the electrical conductivity data with theoretical predictions for melt distribution indicates that the model assuming that the grain boundary is completely wetted by melt is the most preferable melt geometry. The gradual change of conductivity with melt fraction suggests no permeability jump due to melt percolation at a certain melt fraction. The melt fraction of the partial molten region in the upper mantle can be estimated to be 1–3% and ∼ 0.3% for basaltic melt and carbonatite melt, respectively.