Halogen variations through the quenched margin of a MORB lava: Evidence for direct assimilation of seawater during eruption

Michael W. Broadley (1) , Ray. Burgess (2) , Hidenori. Kumagai (3, 4) , Natalie M. Curran (2) , Chris J. Ballentine (5)

1 CRPG - Centre de Recherches Pétrographiques et Géochimiques
2 SEAES - School of Earth, Atmospheric and Environmental Sciences [Manchester]
3 IFREE - Institute for Research on Earth Evolution [Yokosuka]
4 JAMSTEC - Japan Agency for Marine-Earth Science and Technology
5 Department of Earth Sciences [Oxford]

Halogens and noble gases within submarine basaltic glasses are critical tracers of interactions between the surface volatile reservoirs and the mantle. However, as the halogens and noble gases are concentrated within seawater, sediments, and the oceanic crust this makes the original volatile signature of submarine basaltic lavas susceptible to geochemical overprinting. This study combines halogen (Cl, Br, and I), noble gas, and K concentrations within a single submarine basaltic quenched margin to quantify the amount of seawater assimilation during eruption, and to further elucidate the mechanisms of overprinting. The outer sections of the glass rim are enriched in Cl compared to the interior of the margin, which maintains mantle-like Br/Cl, I/Cl, and K/Cl ratios. Low Br/Cl and K/Cl in the outer sections of the basaltic glass margin indicate that the Cl enrichment in the outer glass is derived from the assimilation of a saline brine component with up to 70% of the Cl within the glass being derived from brine assimilation. Atmospheric noble gas contamination is decoupled from halogen contamination with contaminated outer sections maintaining MORB-like ⁴⁰Ar/³⁶Ar, suggesting seawater-derived brine assimilation during eruption is not the dominant source of atmospheric noble gases in submarine basalts. Volatile heterogeneities in submarine basalts introduced during and after eruption, as we have shown in this study, have the potential to expand the range of mantle halogen compositions and only by better understanding these heterogeneities can the Br/Cl and I/Cl variance in mantle derived samples are determined accurately.

Mots clés: halogens; mantle; seawater assimilation; noble gases

Domaines: Planète et Univers [physics]; Sciences de la Terre

Michael W. Broadley, Ray. Burgess, Hidenori. Kumagai, Natalie M. Curran, Chris J. Ballentine. Halogen variations through the quenched margin of a MORB lava: Evidence for direct assimilation of seawater during eruption. Geochemistry, Geophysics, Geosystems, 2017, 18 (7), pp.2413-2428. ⟨10.1002/2016GC006711⟩. ⟨insu-03619401⟩