Discussion of recent papers on carbonated peridotite, bearing on mantle metasomatism and magmatism: an alternative

Details Discussion of recent papers on carbonated peridotite, bearing on mantle metasomatism and magmatism: an alternative Discussion of recent papers on carbonated peridotite, bearing on mantle metasomatism and magmatism: an alternative

Apr 1987

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987e%26psl..82..398e&link_type=abstract

Earth and Planetary Science Letters, Volume 82, Issue 3-4, p. 398-400.

Physics

12

Scientific paper

The experimental study of Olafsson and Eggler [1] is not inconsistent with the model system CaO-MgO-SiO2-CO2, if an alternate topology for peridotite-CO2-H2O is considered. Although peridotite-H2O-CO2 solidi present barriers to ascent of partially-melted peridotite, solidi should be applied to melts with caution. Melts such as kimberlites plausibly can ascend rapidly through fractures without appreciable reaction with peridotitic wallrocks.

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