Continuous eclogite melting and variable refertilisation in upwelling heterogeneous mantle View Full Text


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Article Info

DATE

2015-05

AUTHORS

Anja Rosenthal, Gregory M Yaxley, David H Green, Joerg Hermann, István Kovács, Carl Spandler

ABSTRACT

Large-scale tectonic processes introduce a range of crustal lithologies into the Earth's mantle. These lithologies have been implicated as sources of compositional heterogeneity in mantle-derived magmas. The model being explored here assumes the presence of widely dispersed fragments of residual eclogite (derived from recycled oceanic crust), stretched and stirred by convection in the mantle. Here we show with an experimental study that these residual eclogites continuously melt during upwelling of such heterogeneous mantle and we characterize the melting reactions and compositional changes in the residue minerals. The chemical exchange between these partial melts and more refractory peridotite leads to a variably metasomatised mantle. Re-melting of these metasomatised peridotite lithologies at given pressures and temperatures results in diverse melt compositions, which may contribute to the observed heterogeneity of oceanic basalt suites. We also show that heterogeneous upwelling mantle is subject to diverse local freezing, hybridization and carbonate-carbon-silicate redox reactions along a mantle adiabat. More... »

PAGES

6099

References to SciGraph publications

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  • 2007-10. High-pressure partial melting of gabbro and its role in the Hawaiian magma source in CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
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  • 2008-11. Hydrogen partitioning between melt, clinopyroxene, and garnet at 3 GPa in a hydrous MORB with 6 wt.% H2O in CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
  • 2000-07. Experimental study of the phase and melting relations of homogeneous basalt + peridotite mixtures and implications for the petrogenesis of flood basalts in CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
  • 1982. Reduced Volatiles in the System C-O-H: Implications to Mantle Melting, Fluid Formation, and Diamond Genesis in HIGH-PRESSURE RESEARCH IN GEOPHYSICS
  • 2013-01-02. The oxidation state of the mantle and the extraction of carbon from Earth’s interior in NATURE
  • 1996-07. A possible role for garnet pyroxenite in the origin of the “garnet signature” in MORB in CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
  • 2013-05. Stagnation of subducting slabs in the transition zone due to slow diffusion in majoritic garnet in NATURE GEOSCIENCE
  • 2010-09. Water and its influence on the lithosphere–asthenosphere boundary in NATURE
  • 2013-01-09. Carbon-dioxide-rich silicate melt in the Earth’s upper mantle in NATURE
  • Identifiers

    URI

    http://scigraph.springernature.com/pub.10.1038/srep06099

    DOI

    http://dx.doi.org/10.1038/srep06099

    DIMENSIONS

    https://app.dimensions.ai/details/publication/pub.1035277590

    PUBMED

    https://www.ncbi.nlm.nih.gov/pubmed/25130275


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