Lithium isotopes in hydrothermally altered basalts from Hengill (SW Iceland)

The Li isotope signatures of hydrothermal fluids are remarkably constant (delta Li-7 = 8.0 +/- 1.97 parts per thousand) irrespective of the water/rock ratio (W/R), permeability, temperature or fluid involved (seawater or meteoric). High temperature hydrothermal fluids represent the second most significant source of Li to the ocean, yet the homogeneity of the Li isotopic signatures of this source remains to be explained and in this context, the lack of data for the corresponding altered phases is problematic. We measured Li contents and Li isotope signatures (as well as mineralogy, composition and local fluid temperature) in hyaloclastites collected from a borehole in the Hellisheidi geothermal system (Iceland) which have been altered by high temperature aqueous fluids (from 170 to 300 degrees C). Li is more enriched in the solid phases than the other alkali metals, highlighting its greater ability to be incorporated into secondary phases, especially at high temperatures (>250 degrees C). Mass balance calculations show that the low Li concentrations in hydrothermal fluids are best explained by a high water/rock ratio and a high permeability of this system. The Li isotopic signature of the altered hyaloclastites (delta Li-7 between +1.9 and +4.0 parts per thousand) remains close to the fresh basalt at deep levels and high temperatures (290-300 degrees C) (as measured delta Li-7 range between +3.7 and +4.0 parts per thousand), and decreases at shallower depths and lower temperatures (150-270 degrees C) (delta Li-7 between +1.9 and +3.1 parts per thousand). A mass balance model involving basalt dissolution, secondary phase formation, and successive isotope equilibrium during the migration and the cooling of the percolating fluid was developed. The corresponding apparent mineral-fluid Li isotope fractionation factors resulting from precipitation of secondary phases (Delta Li-7(minerals-fluid)) range between 0 parts per thousand at 300 degrees C and -8.5 parts per thousand at 170 degrees C and highlight a key role of chlorite. Applying the same approach to mid-ridge oceanic hydrothermal systems allows the relatively homogeneous isotope signatures of high temperature fluids of various locations to be explained. (C) 2014 Elsevier B.V. All rights reserved.