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    A reassessment of spectral T e estimation in continental interiors: the case of North America

    128965_PID128965%20A%20reassessment%20of%20spectral.pdf (4.827Mb)
    Access Status
    Open access
    Authors
    Kirby, Jonathan
    Swain, Christopher
    Date
    2009
    Type
    Journal Article
    
    Metadata
    Show full item record
    Citation
    Kirby, Jonathan and Swain, Christopher. 2009. A reassessment of spectral T e estimation in continental interiors: the case of North America. Journal of Geophysical Research-Solid Earth. 114 (B08401).
    Source Title
    Journal of Geophysical Research JGR Solid Earth
    DOI
    10.1029/2009JB006356
    ISSN
    01480227
    Faculty
    Department of Spatial Sciences
    Faculty of Science and Engineering
    The Western Australian School of Mines
    Remarks

    An edited version of this paper was published by AGU. Copyright © 2009 American Geophysical Union.

    Citation: Kirby, J. F. and C. J. Swain (2009), A reassessment of spectral Te estimation in continental interiors: The case of North America, J. Geophys. Res., 114, B08401, doi: 10.1029/2009JB006356.

    URI
    http://hdl.handle.net/20.500.11937/34771
    Collection
    • Curtin Research Publications
    Abstract

    Conventional spectral T e studies use the real part of the admittance between gravity anomalies and topography or, alternatively, the square of the magnitude of the coherency (i.e., coherence). Here we show the utility of treating both the admittance and coherency as complex quantities. Inverting the real parts to estimate T e, we use the imaginary parts to tell if the inversion is biased by noise. One method inverts the square of the real coherency, with the internal-to-total load ratio F derived (as a function of wave number) directly from the gravity and topography. The other method inverts the real part of the admittance assuming that F is wave number-independent. We test the methods using synthetic elastic plate models loaded at the surface and Moho in such a way that the final relief is the actual North American topography. In some of the models we add gravity noise generated by a model having both surface and internal loads such that the final topography is zero and find that both methods are susceptible to noise. Application of the two methods to North America gives T e maps showing substantial agreement except in regions affected by noise, but these are not a dominant part of the total area. Given the suggested mechanisms by which noise might arise, it is not surprising that it is not a more widespread feature of the North American craton. Importantly, both methods show that large parts of the Canadian Shield are characterized by T e > 100 km.

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