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

Takashi Yoshino, Mickael Laumonier, Elizabeth McIsaac, Tomoo Katsura

Research output: Contribution to journalArticle

72 Citations (Scopus)

Abstract

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 1600K at 1.5GPa and up to at least 1650K at 3GPa, 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 (σbulk) and log melt fraction (Φ) can be expressed well by the Archie's law (Archie, 1942) (σbulkmelt=CΦn) 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.

Original languageEnglish
Pages (from-to)593-602
Number of pages10
JournalEarth and Planetary Science Letters
Volume295
Issue number3-4
DOIs
Publication statusPublished - Jul 2010

Fingerprint

Bearings (structural)
Silicates
carbonatite
Carbonates
electrical conductivity
Molten materials
upper mantle
Earth mantle
melt
electrical resistivity
conductivity
Acoustic impedance
silicates
carbonates
olivine
basalt
Grain boundaries
Geometry
mid-ocean ridges
peridotite

Keywords

  • Basalt
  • Carbonatite
  • Electrical conductivity
  • Melt fraction
  • Permeability

ASJC Scopus subject areas

  • Geochemistry and Petrology
  • Geophysics
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science

Cite this

Electrical conductivity of basaltic and carbonatite melt-bearing peridotites at high pressures : Implications for melt distribution and melt fraction in the upper mantle. / Yoshino, Takashi; Laumonier, Mickael; McIsaac, Elizabeth; Katsura, Tomoo.

In: Earth and Planetary Science Letters, Vol. 295, No. 3-4, 07.2010, p. 593-602.

Research output: Contribution to journalArticle

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