The Lithium, Boron and Beryllium Content Of
Published in Geochimica et Cosmochimica Acta 72, issue 22, 5475-5504, 2008 1 which should be used for any reference to this work The Lithium, Boron and Beryllium content of serpentinized peridotites from ODP Leg 209 (Sites 1272A and 1274A): Implications for lithium and boron budgets of oceanic lithosphere Flurin Vils a,*, Laure Pelletier a, Angelika Kalt a, Othmar Mu¨ntener b, Thomas Ludwig c a Institut de Ge´ologie et d’Hydroge´ologie, Universite´ de Neuchaˆtel, Rue Emile-Argand 11, CP 158, CH-2009 Neuchaˆtel, Switzerland b Institut de Mine´ralogie et Ge´ochimie, Universite´ de Lausanne, Anthropole, CH-1015 Lausanne, Switzerland c Mineralogisches Institut, Ruprecht-Karls-Universita¨t Heidelberg, Im Neuenheimer Feld 236, D-69120 Heidelberg, Germany Abstract Despite the key importance of altered oceanic mantle as a repository and carrier of light elements (B, Li, and Be) to depth, its inventory of these elements has hardly been explored and quantified. In order to constrain the systematics and budget of these elements we have studied samples of highly serpentinized (>50%) spinel harzburgite drilled at the Mid-Atlantic Ridge (Fifteen– Twenty Fracture zone, ODP Leg 209, Sites 1272A and 1274A). In-situ analysis by secondary ion mass spectrometry reveals that the B, Li and Be contents of mantle minerals (olivine, orthopyroxene, and clinopyroxene) remain unchanged during serpent- inization. B and Li abundances largely correspond to those of unaltered mantle minerals whereas Be is close to the detection limit. The Li contents of clinopyroxene are slightly higher (0.44–2.8 lggÀ1) compared to unaltered mantle clinopyroxene, and olivine and clinopyroxene show an inverse Li partitioning compared to literature data.
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