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The competition between rates of deformation and solidification in syn-kinematic granitic intrusions : Resolving the pegmatite paradox

dc.contributor.authorButler, Robert W.H.
dc.contributor.authorTorvela, Taija
dc.contributor.institutionUniversity of Aberdeen.Geology and Geophysicsen
dc.contributor.institutionUniversity of Aberdeen.Centre for Energy Transitionen
dc.date.accessioned2019-09-03T23:02:59Z
dc.date.available2019-09-03T23:02:59Z
dc.date.embargoedUntil2019-09-04
dc.date.issued2018-12-01
dc.descriptionWe thank Ian Alsop and Rob Strachan for discussions on the deformation at Torrisdale together with Alan Whittington and Mona-Liza Sirbescu for discussions and sharing manuscripts on melt rheologies and pegmatite crystallization. We also thank Elena Druguet for comments on a draft of these ideas, Luca Menegon and Denis Gapais for vigorous reviews of this paper, Bill Dunne for his editorial sweep-through, and participants at DRT2017 in Inverness for comments, in and out of the field. However, the views expressed here are exclusively those of the authors.en
dc.description.statusPeer revieweden
dc.format.extent13
dc.format.extent34295628
dc.identifier138331891
dc.identifier0ff21661-0c3c-4134-aec7-2c50a171e78a
dc.identifier85053083206
dc.identifier.citationButler, R W H & Torvela, T 2018, 'The competition between rates of deformation and solidification in syn-kinematic granitic intrusions : Resolving the pegmatite paradox', Journal of Structural Geology, vol. 117, pp. 1-13. https://doi.org/10.1016/j.jsg.2018.08.013en
dc.identifier.doi10.1016/j.jsg.2018.08.013
dc.identifier.issn0191-8141
dc.identifier.otherRIS: urn:7CAE982463D2FF8D0B85D639B00E9592
dc.identifier.urihttp://hdl.handle.net/2164/12839
dc.identifier.vol117en
dc.language.isoeng
dc.relation.ispartofJournal of Structural Geologyen
dc.subjectPegmatitesen
dc.subjectMelt-enhanced deformationen
dc.subjectContinental deformationen
dc.subjectRheologyen
dc.subjectQE Geologyen
dc.subject.lccQEen
dc.titleThe competition between rates of deformation and solidification in syn-kinematic granitic intrusions : Resolving the pegmatite paradoxen
dc.typeJournal articleen

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