The eclogite to garnetite transition — Experimental and thermodynamic constraints

Craig R. Bina*, Bernard J. Wood

*Corresponding author for this work

    Research output: Contribution to journalArticle

    21 Citations (Scopus)

    Abstract

    We have found that the forms of the experimentally determined phase diagrams for pyroxene‐garnet transformations require the volume changes for these reactions to be much smaller at 130 kbar (400 km) than at 1 atm. Using these volume data we calculated the width of the eclogite‐garnetite transition in natural quartz tholeiite and alkali olivine basalt compositions taking account of mixing in multicomponent pyroxene and garnet phases. We find that the eclogite‐garnetite transition does not exhibit any discontinuity in bulk sound velocity in the pressure range 110 to 230 kbar. In addition, this velocity, when plotted as a function of pressure, possesses a curvature which is in the opposite sense to that given by the Preliminary Reference Earth Model (PREM). This phase transition, therefore, does not appear to be a satisfactory model for the 400 km seismic discontinuity.

    Original languageEnglish
    Pages (from-to)955-958
    Number of pages4
    JournalGeophysical Research Letters
    Volume11
    Issue number10
    DOIs
    Publication statusPublished - 1984

    Fingerprint Dive into the research topics of 'The eclogite to garnetite transition — Experimental and thermodynamic constraints'. Together they form a unique fingerprint.

  • Cite this