Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/153534
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dc.contributor.authorPalin, Richard.M.en_US
dc.contributor.authorMoore, James Daniel Paulen_US
dc.contributor.authorZhang, Zemingen_US
dc.contributor.authorHuang, Guangyuen_US
dc.contributor.authorWade, Jonen_US
dc.contributor.authorDyck, Brendanen_US
dc.date.accessioned2021-12-07T07:29:25Z-
dc.date.available2021-12-07T07:29:25Z-
dc.date.issued2021-
dc.identifier.citationPalin, R., Moore, J. D. P., Zhang, Z., Huang, G., Wade, J. & Dyck, B. (2021). Mafic Archean continental crust prohibited exhumation of orogenic UHP eclogite. Geoscience Frontiers, 12(5), 101225-. https://dx.doi.org/10.1016/j.gsf.2021.101225en_US
dc.identifier.issn1674-9871en_US
dc.identifier.urihttps://hdl.handle.net/10356/153534-
dc.description.abstractThe absence of ultrahigh pressure (UHP) orogenic eclogite in the geological record older than c. 0.6 Ga is problematic for evidence of subduction having begun on Earth during the Archean (4.0–2.5 Ga). Many eclogites in Phanerozoic and Proterozoic terranes occur as mafic boudins encased within low-density felsic crust, which provides positive buoyancy during subduction; however, recent geochemical proxy analysis shows that Archean continental crust was more mafic than previously thought, having greater proportions of basalt and komatiite than modern-day continents. Here, we show via petrological modelling that secular change in the petrology and bulk composition of upper continental crust would make Archean continental terranes negatively buoyant in the mantle before reaching UHP conditions. Subducted or delaminated Archean continental crust passes a point of no return during metamorphism in the mantle prior to the stabilization of coesite, while Proterozoic and Phanerozoic terranes remain positively buoyant at these depths. UHP orogenic eclogite may thus readily have formed on the Archean Earth, but could not have been exhumed, weakening arguments for a Neoproterozoic onset of subduction and plate tectonics. Further, isostatic balance calculations for more mafic Archean continents indicate that the early Earth was covered by a global ocean over 1 km deep, corroborating independent isotopic evidence for large-scale emergence of the continents no earlier than c. 3 Ga. Our findings thus weaken arguments that early life on Earth likely emerged in shallow subaerial ponds, and instead support hypotheses involving development at hydrothermal vents in the deep ocean.en_US
dc.language.isoenen_US
dc.relation.ispartofGeoscience Frontiersen_US
dc.rights©2021 China University of Geosciences (Beijing) and Peking University. Production and hosting byElsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/)en_US
dc.subjectScience::Geologyen_US
dc.titleMafic Archean continental crust prohibited exhumation of orogenic UHP eclogiteen_US
dc.typeJournal Articleen
dc.contributor.researchEarth Observatory of Singaporeen_US
dc.identifier.doi10.1016/j.gsf.2021.101225-
dc.description.versionPublished versionen_US
dc.identifier.scopus2-s2.0-85107692227-
dc.identifier.issue5en_US
dc.identifier.volume12en_US
dc.identifier.spage101225en_US
dc.subject.keywordsArcheanen_US
dc.subject.keywordsEclogiteen_US
dc.description.acknowledgementThe authors are grateful for comments on earlier version of thiswork by Clare Warren, Alan Hastie, and Daniel Wiemer, and formalcomments on this most recent version by two anonymous review-ers. JDPM acknowledges support from Marsden grant 14-VUW-085, Royal Society of New Zealand. Codes for reproducing the iso-static balance calculation and yield strength envelopes may befound at www.jamesdpmoore.comen_US
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