Dunite distribution in the Oman ophiolite: Implications for melt flux through porous dunite conduits

Publication Status is "Submitted" Or "In Press: 
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Year of Publication: 
2002
Editor: 
Journal Title: 
Geochemistry Geophysics Geosystems
Journal Date: 
Nov 6
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Tertiary Title: 
Volume: 
3
Issue: 
Pages: 
-
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ISBN Number: 
1525-2027
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Edition: 
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Accession Number: 
ISI:000179077900001
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Abstract: 

[1] Dunites in the mantle section of the Oman ophiolite represent conduits for chemically isolated melt transport through the shallow mantle beneath oceanic spreading centers. These dunite melt conduits exhibit a scale-invariant power law relationship between width and cumulative abundance, as measured over 4 orders of magnitude. We use this size/frequency distribution to assess several hypotheses for dunite formation and estimate the total melt flux that a dunite network can accommodate beneath an oceanic spreading center. Dunites, measured from one-dimensional lithologic sections and digital image mosaics at a variety of length scales, range in width from similar to3 mm to similar to100 m and follow a power law with a slope of similar to1.1. Extrapolation of the power law predicts that dunites as wide as 3.5 km may exist in the melting region beneath a mid-ocean ridge. Alternatively, perhaps the widest dunites we observe ( 100 m) represent a maximum size. Modeling of dunites as diffusive reaction zones around melt-filled hydrofractures cannot explain the existence of dunites wider than similar to10 m in Oman. Instead, dunites may represent high porosity conduits formed by reactive porous flow. Using the observed size/frequency relationship, the assumption that dunites form a coalescing network and the requirement that flux is conserved where dunites merge, we estimate the total flux through a porous dunite network and the fraction of that flux that remains chemically isolated. Our flux model predicts that the porosity in a dunite scales with the width. For maximum porosities of similar to1-4% in the widest dunites, a network of porous dunite conduits with the abundances observed in Oman can supply a sufficient flux of melt (of which >95% remains chemically unequilibrated with shallow residual peridotites) to satisfy the observed mid-ocean ridge flux.

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612LUTimes Cited:17Cited References Count:61

DOI: 
Doi 10.1029/2001gc000289