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    The coherence method using a thin anisotropic elastic plate model

    117396_4002_Swain_GRL_03b.pdf (135.7Kb)
    Access Status
    Open access
    Authors
    Swain, Christopher
    Kirby, Jonathan
    Date
    2003
    Type
    Journal Article
    
    Metadata
    Show full item record
    Citation
    Swain, Christopher and Kirby, Jonathan. 2003. The coherence method using a thin anisotropic elastic plate model. Geophysical Research Letters. 30 (19): pp. 2014-2019.
    Source Title
    Geophysical Research Letters
    DOI
    10.1029/2003GL018350
    ISSN
    00948276
    Faculty
    Department of Spatial Sciences
    Faculty of Science and Engineering
    The Western Australian School of Mines
    Remarks

    Copyright © 2003 American Geophysical Union.

    Publisher’s Citation: Swain, C. J., and J. F. Kirby (2003), The coherence method using a thin anisotropic elastic plate model, Geophysical Research Letters, Vol. 30 (19), 2014, doi: 10.1029/2003GL018350.

    URI
    http://hdl.handle.net/20.500.11937/36148
    Collection
    • Curtin Research Publications
    Abstract

    The coherence method, based on the statistical correlation between gravity and topography, has beenwidely used to estimate the effective elastic thickness of the continental lithosphere and its variations. By far the majority of studies have assumed an isotropic lithosphere, but several papers have inferred anisotropy from differences in the observed coherence (or admittance) functions in different directions. However, none have used an anisotropic model to fit the coherence. We show how the simplest model of elastic anisotropy (an orthotropic thin plate) can be incorporated into both forward and inverse modeling algorithms, using an appropriate approximation in the partial differential equation for the flexure of such a plate.

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