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GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,
VOL. 3,
1007,
20 PP., 2002
doi:10.1029/2001GC000178 [Citation]
Behavior of Li and its isotopes during serpentinization of oceanic peridotites
CRPG-CNRS, 15 rue Notre-Dame des Pauvres, Vandoeuvre les Nancy Cedex, 54501 France
CRPG-CNRS, 15 rue Notre-Dame des Pauvres, Vandoeuvre les Nancy Cedex, 54501 France
CRPG-CNRS, 15 rue Notre-Dame des Pauvres, Vandoeuvre les Nancy Cedex, 54501 France
Department of Earth Sciences, The Open University, Walton Hall, Milton Keynes, MK7 6AA, England
Laboratoire de Geochimie des Isotopes Stables - IPGP and Universite Denis Diderot (Paris 7), 2 place Jussieu, Paris Cedex 05 75251 France
Laboratoire de Petrologie - CNRS UPRES A 7058 Universite Pierre et Marie Curie, Case 110 4 place Jussieu, Paris Cedex 05 75252 France
Analyses of Li and Li isotopes in serpentinized peridotites have been performed using Thermo-Ionisation Mass Spectrometry (TIMS) and Secondary Ion Mass Spectrometry (SIMS) techniques on samples collected from the southwest Indian Ridge (SWIR). In the bulk samples, Li concentrations range from 0.6 to 8.2 ppm, while whole rock δ6Li values range from −2.9 to −14‰. In situ analyses display a greater range in both Li concentration (0.1–19.5 ppm) and Li isotopic composition (−27 to +19‰), with the serpentinized portions having higher Li concentrations than the associated relict phases. These variations may reflect changes in Li partitioning and isotopic fractionation between serpentine and fluid with temperature and water/rock ratio. They may also be explained by changes in the composition of the serpentinizing fluid over the course of serpentinization. As the serpentine forms by interaction with a circulating fluid, it preferentially removes 6Li, causing the Li in the fluid to become isotopically heavier. The isotopic composition of the initial hydrothermal fluid is dominated by basalt-derived Li, which easily overwhelms the very low Li content originally present in seawater. As this fluid circulates through ultramafic rocks, it induces the formation of serpentine that incorporates this mantle-derived Li. Hence, Li in serpentine is mainly derived from oceanic crust rather than from seawater and serpentinization involves Li recycling within this crust. Consequently, Li isotopes are good tracers of the hydrothermal contribution in serpentinizing fluid. These results imply that serpentinized peridotites are probably only a minor sink of oceanic Li.
Received 10 May 2001; accepted 17 September 2001; published 31 January 2002.
Citation: (2002), Behavior of Li and its isotopes during serpentinization of oceanic peridotites, Geochem. Geophys. Geosyst., 3(1), 1007, doi:10.1029/2001GC000178.
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