Seismic anisotropy and mantle structure of the Rae craton, central Canada, from joint interpretation of SKS splitting and receiver functions

► Seismic anisotropy occurs in either one or two layers beneath northern Hudson Bay, Canada. ► The deeper layer's fabric appears aligned with plate motion. ► The shallow one represents fossil structure from Proterozoic or Archean tectonics. ► Seismic discontinuities occur at 50–130km depths. Ea...

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Bibliographic Details
Published inPrecambrian research Vol. 232; pp. 189 - 208
Main Authors Snyder, D.B., Berman, R.G., Kendall, J.-M., Sanborn-Barrie, M.
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.07.2013
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