Dube, Jean-MichelDarbyshire, FionaLiddell, MitchStephenson, RandellOakey, Gordon N.2021-06-162021-06-162020-08-20Dube, J-M, Darbyshire, F, Liddell, M, Stephenson, R & Oakey, G N 2020, 'Seismic anisotropy of the Canadian High Arctic : evidence from shear-wave splitting', Tectonophysics, vol. 789, 228524. https://doi.org/10.1016/j.tecto.2020.2285240040-1951ORCID: /0000-0003-4868-8601/work/81609522https://hdl.handle.net/2164/16681FD is supported by the Natural Sciences and Engineering Research Council of Canada (NSERC/CRSNG) through its Discovery Grant and Canada Research Chair programmes [10.13039/501100000038](341802-2013-RGPIN). Data from the ELLITE stations and some of the long-term stations (Scripps Inst. Oceanography, 1986; Stephenson et al., 2013) are available through the IRIS Data Management Center; the remaining Canadian data are available through the Canadian National Data Centre, Natural Resources Canada (Geological Survey of Canada, 1989). ELLITE instrumentation was loaned to the project by SEIS-UK and the project received support from De Beers Canada and the University of Aberdeen. The ELLITE project was carried out as part of the Circum-Arctic Lithosphere Evolution (CALE) programme, and supported by Natural Resources Canada's GEM-1 programme, which also supported JMD's MSc funding. We thank the Editor and the three reviewers for their helpful comments which improved the manuscript.139936109engseismic anisotropyshear wave splittingCanadian High Articlithospheric deformationSeismic anisotropyCanadian High ArcticLithospheric deformationShear wave splittingQE GeologyEarth-Surface ProcessesGeophysicsQEJournal article10.1016/j.tecto.2020.228524http://www.scopus.com/inward/record.url?scp=85086722226&partnerID=8YFLogxK789