Nickel Isotope Fractionation During Tropical Weathering of Ultramafic Rocks
Chemical Geology 402 (2015) 68–76 Contents lists available at ScienceDirect Chemical Geology journal homepage: www.elsevier.com/locate/chemgeo Nickel isotope fractionation during tropical weathering of ultramafic rocks G. Ratié a,b, D. Jouvin a,J.Garnierb, O. Rouxel c,S.Miskaa, E. Guimarães b,L.CruzVieirab, Y. Sivry d,I.Zelanod, E. Montarges‐Pelletier e,F.Thilf, C. Quantin a,⁎ a UMR 8148GEOPS, Université Paris Sud — CNRS, 91405 Orsay Cedex, France b UnB, IG/GMP-ICC Centro, Campus Universitario Darcy Ribeiro, 70910-970, Brasilia DF, Brazil c IFREMER, Centre de Brest, Unité Géosciences Marines, 29280 Plouzané, France d Institut de Physique du Globe de Paris, Sorbonne Paris Cité, Université Paris Diderot, UMR 7154 CNRS, F-75005 Paris, France e Laboratoire Interdisciplinaire des Environnements Continentaux, UMR 7360 CNRS Université de Lorraine, 15 Avenue du Charmois, 54500 Vandœuvre-lès-Nancy, France f Laboratoire des Sciences du Climat et de l'Environnement (LSCE/IPSL), UMR 8212 (CEA/CNRS/UVSQ), Domaine du CNRS, Avenue de la Terrasse, Bat 12, 91198 Gif-sur-Yvette, France article info abstract Article history: Although Ni isotopes have been shown to be significantly fractionated in terrestrial samples, their use in conti- Received 13 May 2014 nental environmental studies has not yet been evaluated. The present study focuses on an ultramafic(UM)massif Received in revised form 25 February 2015 (Barro Alto, Goiás, Brazil) because such areas are naturally rich in Ni. We present developed lateritic weathering Accepted 27 February 2015 profiles. The goal of the study is to evaluate the potential of using Ni isotopes in environmental continental stud- Available online 7 March 2015 ies by combining its isotopic signature with mineralogy, in order to better understand the geochemical cycling of Editor: Michael E.
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