The significance of seismic wavespeed minima and thermal maxima in the mantle and the role of dynamic melting

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Sammis, Charles G. [1 ]
Anderson, Don L. [1 ]
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[1] Department of Earth Sciences, University of Southern California, Los Angeles,CA,90089-0740, United States
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10.1130/2015.251401
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  • [1] Reconciling dynamic and seismic models of Earth's lower mantle: The dominant role of thermal heterogeneity
    Davies, D. Rhodri
    Goes, S.
    Davies, J. H.
    Schuberth, B. S. A.
    Bunge, H. -P.
    Ritsema, J.
    [J]. EARTH AND PLANETARY SCIENCE LETTERS, 2012, 353 : 253 - 269
  • [2] How dynamic weakening makes faults stronger: The role of melting in post-seismic healing
    Griffith, W. Ashley
    [J]. GEOLOGY, 2016, 44 (12) : 1063 - 1064
  • [3] Thermochemical interpretation of 1-D seismic data for the lower mantle: The significance of nonadiabatic thermal gradients and compositional heterogeneity
    Cobden, Laura
    Goes, Saskia
    Ravenna, Matteo
    Styles, Elinor
    Cammarano, Fabio
    Gallagher, Kerry
    Connolly, James A. D.
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2009, 114
  • [4] The role of thermal effect on mantle seismic anomalies under Laurentia and Fennoscandia from observations of Glacial Isostatic Adjustment
    Wu, Patrick
    Wang, Hansheng
    Steffen, Holger
    [J]. GEOPHYSICAL JOURNAL INTERNATIONAL, 2013, 192 (01) : 7 - 17