Formulations for Simulating the Multiscale Physics of Magma Ascent

Craig O'Neill*, Marc Spiegelman

*Corresponding author for this work

    Research output: Chapter in Book/Report/Conference proceedingChapter

    1 Citation (Scopus)

    Abstract

    Melt migration from a mantle source to eventual eruption may involve a variety of processes operating over a range of scales. For instance, melt ascent begins with grain-scale interactions, which, for larger fluxes may be described by permeable flow. Field evidence demonstrates that melt eventually coalesces to forms vein or dyke networks, which may rapidly ascend and be erupted, or be emplaced at depth, where they may feed into crustal magma chambers. A variety of mathematical formulations exist to describe these processes at different scales, and this contribution draws these diverse approaches together to form a framework for quantifying magma ascent from source to surface.

    Original languageEnglish
    Title of host publicationTimescales of Magmatic Processes
    Subtitle of host publicationFrom Core to Atmosphere
    EditorsAnthony Dosseto, Simon P. Turner, James A. Van Orman
    Place of PublicationChichester, West Sussex, UK
    PublisherJohn Wiley & Sons
    Pages87-101
    Number of pages15
    ISBN (Electronic)9781444328509
    ISBN (Print)9781444332605, 1444332600
    DOIs
    Publication statusPublished - 30 Nov 2010

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