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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Published in | Precambrian research Vol. 232; pp. 189 - 208 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
01.07.2013
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Subjects | |
Online Access | Get full text |
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