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

Earthquakes recorded at 36 stations in Nunavut between 1992 and 2011 and analyzed jointly using receiver-function and SKS-splitting techniques indicate the presence of multiple, dipping anisotropic layers in the lithosphere beneath the northern Hudson Bay and Baffin Island region. Prominent disconti...

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Bibliographic Details
Published in:Precambrian Research
Main Authors: Snyder, D. B., Berman, R. G., Kendall, J. -M., Sanborn-Barrie, M.
Format: Article in Journal/Newspaper
Language:English
Published: 2013
Subjects:
Hudson Bay
SKS anisotropy
Mantle lithosphere
Rae craton
Mantle discontinuities
WESTERN CHURCHILL PROVINCE
TRANS-HUDSON OROGEN
SNOWBIRD TECTONIC ZONE
COMMITTEE BAY BELT
U-PB
AZIMUTHAL ANISOTROPY
BAFFIN-ISLAND
WAVE
GEOCHRONOLOGY
LAURENTIA
Baffin Island
Canada
Committee Bay
Hudson
Nunavut
Rae
Southampton Island
Baffin
Online Access:https://hdl.handle.net/1983/99052e86-09dd-41a0-aafd-a18297dbd3d3
https://research-information.bris.ac.uk/en/publications/99052e86-09dd-41a0-aafd-a18297dbd3d3
https://doi.org/10.1016/j.precamres.2012.03.003
Description
Summary:Earthquakes recorded at 36 stations in Nunavut between 1992 and 2011 and analyzed jointly using receiver-function and SKS-splitting techniques indicate the presence of multiple, dipping anisotropic layers in the lithosphere beneath the northern Hudson Bay and Baffin Island region. Prominent discontinuities indicate layers interpreted to dip at 6-30 degrees at depths between 50 and 150 km beneath ten of the stations. One set of regionally continuous discontinuities in anisotropic fabric in the southeastern Rae craton dip gently southeast consistent with underthrusting beneath the Hearne and Meta Incognita-Sugluk blocks. SKS splitting recorded at twelve stations indicate patterns characteristic of two layers of anisotropic fabric. The deeper fabric as well as the single fast polarization direction recorded at other stations appears aligned with recent plate motion. The shallower fabric orientations at stations on and south of Southampton Island in northern Hudson Bay are consistent with known crustal fabric orientations formed during early (pre-1.85 Ga) stages of the Hudsonian orogeny. The shallower fabric north and west of Southampton Island has a more northerly orientation and is associated with west-dipping discontinuities that may correspond to Neoarchean accretion of the Mesoarchean north Rae domain to the central Rae domain. Crown Copyright (C) 2012 Published by Elsevier B.V. All rights reserved.

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