BIROn - Birkbeck Institutional Research Online

    The seismic signature of Upper‐Mantle Plumes: application to the Northern East African Rift

    Civiero, C. and Armitage, J.J. and Goes, S. and Hammond, James O.S. (2019) The seismic signature of Upper‐Mantle Plumes: application to the Northern East African Rift. Geochemistry, Geophysics, Geosystems 20 (12), pp. 6106-6122. ISSN 1525-2027.

    manuscript_revised.pdf - Author's Accepted Manuscript

    Download (8MB) | Preview


    Several seismic and numerical studies proposed that below, some hotspots upper‐mantle plumelets rise from a thermal boundary layer below 660 km depth, fed by a deeper plume source. We recently found tomographic evidence of multiple upper‐mantle upwellings, spaced by several 100 km, rising through the transition zone below the northern East African Rift. To better test this interpretation, we run 3‐D numerical simulations of mantle convection for Newtonian and non‐Newtonian rheologies, for both thermal instabilities rising from a lower boundary layer, and the destabilization of a thermal anomaly placed at the base of the box (700–800 km depth). The thermal structures are converted to seismic velocities using a thermodynamic approach. Resolution tests are then conducted for the same P and S data distribution and inversion parameters as our traveltime tomography. The Rayleigh Taylor models predict simultaneous plumelets in different stages of evolution rising from a hot layer located below the transition zone, resulting in seismic structure that looks more complex than the simple vertical cylinders that are often anticipated. From the wide selection of models tested, we find that the destabilization of a 200 °C, 100 km thick thermal anomaly with a non‐Newtonian rheology, most closely matches the magnitude and the spatial and temporal distribution of the anomalies below the rift. Finally, we find that for reasonable upper‐mantle viscosities, the synthetic plume structures are similar in scale and shape to the actual low‐velocity anomalies, providing further support for the existence of upper‐mantle plumelets below the northern East African Rift.


    Item Type: Article
    Additional Information: Accepted for publication. Copyright American Geophysical Union. Further reproduction or electronic distribution is not permitted.
    Keyword(s) / Subject(s): mantle plumes, Rayleigh Taylor, thermal anomaly, tomography, dynamic modeling, thermal boundary layer
    School: Birkbeck Faculties and Schools > Faculty of Science > School of Natural Sciences
    Depositing User: James Hammond
    Date Deposited: 02 Jan 2020 12:09
    Last Modified: 02 Aug 2023 17:56


    Activity Overview
    6 month trend
    6 month trend

    Additional statistics are available via IRStats2.

    Archive Staff Only (login required)

    Edit/View Item Edit/View Item