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Boron, lithium and strontium isotopes as tracers of seawater–serpentinite interaction at Mid-Atlantic ridge, ODP Leg 209
Auteur(s)
Vils, Flurin
Tonarini, Sonia
Seitz, Hans-Michael
Date de parution
2009
In
Earth and Planetary Science Letters, Elsevier, 2009/386/3-4/414-425
Résumé
Spinel harzburgites from ODP Leg 209 (Sites 1272A, 1274A) drilled at the Mid-Atlantic ridge between 14°N and 16°N are highly serpentinized (50–100%), but still preserve relics of primary phases (olivine ≥ orthopyroxene >> clinopyroxene). We determined whole-rock B and Li isotope compositions in order to constrain the effect of serpentinization on δ<sup>11</sup>B and δ<sup>7</sup>Li. Our data indicate that during serpentinization Li is leached from the rock, while B is added. The samples from ODP Leg 209 show the heaviest δ<sup>11</sup>B (+ 29.6 to + 40.52‰) and lightest δ<sup>7</sup>Li (− 28.46 to + 7.17‰) found so far in oceanic mantle. High <sup>87</sup>Sr/<sup>86</sup>Sr ratios (0.708536 to 0.709130) indicate moderate water/rock ratios (3 to 273, on the average 39), in line with the high degree of serpentinization observed. <br> Applying the known fractionation factors for <sup>11</sup>B/<sup>10</sup>B and <sup>7</sup>Li/<sup>6</sup>Li between seawater and silicates, serpentinized peridotite in equilibrium with seawater at conditions corresponding to those of the studied drill holes (pH: 8.2; temperature: 200 °C) should have δ<sup>11</sup>B of + 21.52‰ and δ<sup>7</sup>Li of + 9.7‰. As the data from ODP Leg 209 are clearly not in line with this, we modelled a process of seawater–rock interaction where δ<sup>11</sup>B and δ<sup>7</sup>Li of seawater evolve during penetration into the oceanic plate. Assuming chemical equilibrium between fluid and a rock with δ<sup>11</sup>B and δ<sup>7</sup>Li of ODP Leg 209 samples, we obtain δ<sup>11</sup>B and δ<sup>7</sup>Li values of + 50 to + 60‰, − 2 to + 12‰, respectively, for the coexisting fluid. In the oceanic domain, no hydrothermal fluids with such high δ<sup>11</sup>B have yet been found, but are predicted by theoretical calculations. Combining the calculated water/rock ratios with the δ<sup>7</sup>Li and δ<sup>11</sup>B evolution in the fluid, shows that modification of δ<sup>7</sup>Li during serpentinization requires higher water/rock ratios than modification of δ<sup>11</sup>B. <br> Extremely heavy δ<sup>11</sup>B in serpentinized oceanic mantle can potentially be transported into subduction zones, as the B budget of the oceanic plate is dominated by serpentinites. Extremely light δ<sup>7</sup>Li is unlikely to survive as the Li budget is dominated by the oceanic crust, even at small fractions.
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journal article
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