3-D multi-observable probabilistic inversion for the compositional and thermal structure of the lithosphere and upper mantle.

II: General methodology and resolution analysis

J. C. Afonso*, J. Fullea, Y. Yang, J. A.D. Connolly, A. G. Jones

*Corresponding author for this work

    Research output: Contribution to journalArticle

    50 Citations (Scopus)

    Abstract

    Here we present a 3-D multi-observable probabilistic inversion method, particularly designed for high-resolution (regional) thermal and compositional mapping of the lithosphere and sub-lithospheric upper mantle that circumvents the problems associated with traditional inversion methods. The key aspects of the method are as follows: (a) it exploits the increasing amount and quality of geophysical datasets; (b) it combines multiple geophysical observables (Rayleigh and Love dispersion curves, body-wave tomography, magnetotelluric, geothermal, petrological, gravity, elevation, and geoid) with different sensitivities to deep/shallow, thermal/compositional anomalies into a single thermodynamic- geophysical framework; (c) it uses a general probabilistic (Bayesian) formulation to appraise the data; (d) no initial model is needed; (e) compositional a priori information relies on robust statistical analyses of a large database of natural mantle samples; and (f) it provides a natural platform to estimate realistic uncertainties. In addition, the modular nature of the method/algorithm allows for incorporating or isolating specific forward operators according to available data. The strengths and limitations of the method are thoroughly explored with synthetic models. It is shown that the a posteriori probability density function (i.e., solution to the inverse problem) satisfactorily captures spatial variations in bulk composition and temperature with high resolution, as well as sharp discontinuities in these fields. Our results indicate that only temperature anomalies of ΔT a 150°C and large compositional anomalies of ΔMg# > 3 (or bulk ΔAl 2O3 > 1.5) can be expected to be resolved simultaneously when combining high-quality geophysical data. This resolving power is sufficient to explore some long-standing problems regarding the nature and evolution of the lithosphere (e.g., vertical stratification of cratonic mantle, compositional versus temperature signatures in seismic velocities, etc) and offers new opportunities for joint studies of the structure of the upper mantle with unprecedented resolution.

    Original languageEnglish
    Pages (from-to)1650-1676
    Number of pages27
    JournalJournal of Geophysical Research: Solid Earth
    Volume118
    Issue number4
    DOIs
    Publication statusPublished - 1 Apr 2013

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