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• W2023900890 abstract "Research Article| July 01, 2004 Quest for palladium: Application of the Groves hypothesis to Precambrian terranes of northeast North America Michel Gauthier; Michel Gauthier 1Département des Sciences de la Terre, Université du Québec à Montréal, c.p. 8888, succ. “Centre-Ville,” Montréal, Québec H3C 3P8, Canada Search for other works by this author on: GSW Google Scholar Stephen Gardoll; Stephen Gardoll 2Centre for Global Metallogeny, Department of Geology and Geophysics, University of Western Australia, 35 Stirling Highway, Crawley, Western Australia 6009, Australia Search for other works by this author on: GSW Google Scholar Jean-Clair Duchesne Jean-Clair Duchesne 3Département de Géologie, Université de Liège, B-4000 Sart-Tilman, Belgium Search for other works by this author on: GSW Google Scholar Geology (2004) 32 (7): 593–596. https://doi.org/10.1130/G20293.1 Article history received: 05 Nov 2003 rev-recd: 19 Mar 2004 accepted: 24 Mar 2004 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Michel Gauthier, Stephen Gardoll, Jean-Clair Duchesne; Quest for palladium: Application of the Groves hypothesis to Precambrian terranes of northeast North America. Geology 2004;; 32 (7): 593–596. doi: https://doi.org/10.1130/G20293.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract A compilation of all types of magmatic deposits in Precambrian terranes of northeast North America revealed a continental-scale metallic zonation. Nickel is homogeneously distributed. Palladium and chromite are centered on the Archean craton, as predicted by the Groves hypothesis, whereas low-Ti Cu-U–rare earth element iron oxide deposits occur just south and east of the Archean and Paleoproterozoic margin, within the Grenville province. Ti is concentrated along this margin in association with anorthosite. Nickel is still abundant there, but palladium and chromite are remarkably absent. This Grenvillian Ni-Pd-Cr paradox suggests that the fractionation process invoked in the classical plume model is inadequate to explain the geochemical characteristics of the anorthosite parental magmas. The crustal-tongue melting model seems to better explain the metallic zonation observed at the margin of the Archean and Proterozoic terranes. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2023900890 title "Quest for palladium: Application of the Groves hypothesis to Precambrian terranes of northeast North America" @default.
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