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dc.contributor.authorSpencer, Christopher J.
dc.contributor.authorCawood, Peter A.
dc.contributor.authorHawkesworth, Chris J.
dc.contributor.authorPrave, Anthony R.
dc.contributor.authorRoberts, Nick M. W.
dc.contributor.authorHorstwood, Matthew S. A.
dc.contributor.authorWhitehouse, Martin J.
dc.identifier.citationSpencer , C J , Cawood , P A , Hawkesworth , C J , Prave , A R , Roberts , N M W , Horstwood , M S A & Whitehouse , M J 2015 , ' Generation and preservation of continental crust in the Grenville Orogeny ' , Geoscience Frontiers , vol. 6 , no. 3 , pp. 357-372 .
dc.identifier.otherPURE: 243532267
dc.identifier.otherPURE UUID: 973eef65-26ab-49a3-8008-036fe1c863ca
dc.identifier.otherScopus: 84927970968
dc.identifier.otherWOS: 000354594600002
dc.identifier.otherORCID: /0000-0002-4614-3774/work/64033699
dc.description.abstractDetrital zircons from modern sediments display an episodic temporal distribution of U-Pb crystallization ages forming a series of 'peaks' and 'troughs'. The peaks are interpreted to represent either periods of enhanced generation of granitic magma perhaps associated with mantle overturn and superplume events, or preferential preservation of continental crust during global collisional orogenesis. The close association of those peaks with the assembly of supercontinents implies a causal relationship between collisional orogenesis and the presence of zircon age peaks. Here these two end-member models (episodic periodicity of increased magmatism versus selective preservation during collisional orogenesis) are assessed using U-Pb, Hf, and O analysis of detrital zircons from sedimentary successions deposited during the ∼1.3-1.1 Ga accretionary, ∼1.1-0.9 Ga collisional, and <0.9 Ga extensional collapse phases of the Grenville orogenic cycle in Labrador and Scotland. The pre-collisional, accretionary stage provides a baseline of continental crust present prior to orogenesis and is dominated by Archean and Paleoproterozoic age peaks associated with pre-1300 Ma Laurentian geology. Strata deposited during the Grenville Orogeny display similar Archean and Paleoproterozoic detrital populations along with a series of broad muted peaks from ∼1500 to 1100 Ma. However, post-collisional sedimentary successions display a dominant age peak between 1085 and 985 Ma, similar to that observed in modern North American river sediments. Zircons within the post-orogenic sedimentary successions have progressively lower εHf and higher δ18O values from ∼1800 to ∼1200 Ma whereupon they have higher εHf and δ18O within the dominant 1085-985 Ma age peak. Furthermore, the Lu-Hf isotopic profile of the Grenville-related age peak is consistent with significant assimilation and contamination by older crustal material. The timing of this dominant age peak coincides with the peak of metamorphism and magmatism associated with the Grenville Orogeny, which is a typical collisional orogenic belt. The change from broad muted age peaks in the syn-orogenic strata to a single peak in the post-orogenic sedimentary successions and in the modern river sediments implies a significant shift in provenance following continental collision. This temporal change in provenance highlights that the source(s), from which detrital zircons within syn-orogenic strata were derived, was no longer available during the later stages of the accretionary and collisional stages of the orogenic cycle. This may reflect some combination of tectonic burial, erosion, or possibly recycling into the mantle by tectonic erosion of the source(s). During continental collision, the incorporated continental crust is isolated from crustal recycling processes operative at subduction margins. This tectonic isolation combined with sedimentary recycling likely controls the presence of the isotopic signature associated with the Grenville Orogeny in the modern Mississippi and Appalachian river sediments. These results imply that zircon age peaks, which developed in conjunction with supercontinents, are the product of selective crustal preservation resulting from collisional orogenesis.
dc.relation.ispartofGeoscience Frontiersen
dc.rights© 2014 China University of Geosciences (Beijing) and Peking University. Production and hosting by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (
dc.subjectContinental crusten
dc.subjectGrenville Orogenyen
dc.subjectCrustal preservationen
dc.subjectGE Environmental Sciencesen
dc.subjectEarth and Planetary Sciences(all)en
dc.titleGeneration and preservation of continental crust in the Grenville Orogenyen
dc.typeJournal articleen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews. Earth and Environmental Sciencesen
dc.contributor.institutionUniversity of St Andrews. School of Geography and Geosciencesen
dc.contributor.institutionUniversity of St Andrews. Scottish Oceans Instituteen
dc.contributor.institutionUniversity of St Andrews. St Andrews Isotope Geochemistryen
dc.contributor.institutionUniversity of St Andrews. School of Earth & Environmental Sciencesen
dc.contributor.institutionUniversity of St Andrews. Marine Alliance for Science & Technology Scotlanden
dc.contributor.institutionUniversity of St Andrews. St Andrews Sustainability Instituteen
dc.description.statusPeer revieweden

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