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The formation of Laurentia : Evidence from shear wave splitting

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dc.contributor.authorLiddell, Mitch V
dc.contributor.authorBastow, Ian
dc.contributor.authorDarbyshire, Fiona
dc.contributor.authorGilligan, Amy
dc.contributor.authorPugh, Steven
dc.contributor.institutionUniversity of Aberdeen.Geography & Environmenten
dc.date.accessioned2017-10-27T15:31:07Z
dc.date.available2017-10-27T15:31:07Z
dc.date.issued2017-12-01
dc.descriptionThe authors would like to thank A. Walker for invaluable help understanding the MSAT forward modelling code, as well as A. Boyce, L. Petrescu, and C. Ogden of the ICcratons group for numerous enlightening conversations about Canadian Precam- brian geology and beyond. M.V. Liddell is funded by an Imperial College President’s Scholarship. F.A. Darbyshire is supported by the Natural Sciences and Environment Research Council of Canada through their Discovery Grant and Canada Research Chair programmes.en
dc.description.statusPeer revieweden
dc.format.extent9
dc.format.extent4166164
dc.identifier108997308
dc.identifier89195d69-d516-452c-b8d7-63995826dbaf
dc.identifier85032673162
dc.identifier.citationLiddell, M V, Bastow, I, Darbyshire, F, Gilligan, A & Pugh, S 2017, 'The formation of Laurentia : Evidence from shear wave splitting', Earth and Planetary Science Letters, vol. 479, pp. 170-178. https://doi.org/10.1016/j.epsl.2017.09.030en
dc.identifier.doi10.1016/j.epsl.2017.09.030
dc.identifier.issn0012-821X
dc.identifier.urihttp://hdl.handle.net/2164/9518
dc.identifier.vol479en
dc.language.isoeng
dc.relation.ispartofEarth and Planetary Science Lettersen
dc.subjectlithosphereen
dc.subjectSKSen
dc.subjectshear wave splittingen
dc.subjectHudson Bayen
dc.subjectPrecambrian tec- 22 tonicsen
dc.subjectanisotropic modellingen
dc.subjectTrans-Hudson Orogenen
dc.subjectNagssugtoqidian Orogenen
dc.subjectcratonsen
dc.subjectseismic anisotropyen
dc.subjectLaurentiaen
dc.subjectQE Geologyen
dc.subject.lccQEen
dc.titleThe formation of Laurentia : Evidence from shear wave splittingen
dc.typeJournal articleen

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