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Tracing helium isotope compositions from mantle source to fumaroles at Oldoinyo Lengai volcano, Tanzania

Mollex, G. ; Füri, E. ; Burnard, P. ; Zimmermann, L. ; Chazot, G. ; Kazimoto, E.O. ; Marty, B. ; France, L., Chemical Geology

Tracing helium isotope compositions from mantle source to fumaroles at Oldoinyo Lengai volcano, Tanzania

Mollex, G. ; Füri, E. ; Burnard, P. ; Zimmermann, L. ; Chazot, G. ; Kazimoto, E.O. ; Marty, B. ; France, L.

Chemical Geology, 480, 66-74

Abstract :

Oldoinyo Lengai is the only volcano on Earth currently erupting natrocarbonatites, of which the source and genesis remain controversial. Cognate xenoliths and fumaroles were sampled at the summit of Oldoinyo Lengai, and deep crustal xenoliths from Oltatwa maar, in 2010 and 2014, after the 2007–2008 sub-Plinian eruption. The summit cognate xenoliths provide direct information on the isotopic composition of the mid-crustal magma chamber that was active during the 2007–2008 explosive eruption. Cognate xenolith-hosted pyroxenes from Oldoinyo Lengai have an average 3He/4He =6.58 ± 0.46 RA, similar to values from nearby silicate volcanoes (4.95–7.30 RA), and reflecting a sub-continental lithospheric mantle (SCLM) signature. This similarity implies that Oldoinyo Lengai carbonatites form from a similar mantle reservoir as the nearby silicate volcanoes. We identify SCLM, metasomatized by fluids/melts derived from the depleted convective mantle, as the common source of magmas in the Arusha volcanic province. Fumarole measurements highlight that fumarolic 3He/4He values have been relatively constant since at least 1988, indicating that dramatic changes to the crater region morphology during the 2007–2008 eruption did not affect the architecture of the hydrothermal system, which is probably connected to the crustal magma chamber(s). Moreover, the similarity between 3He/4He values from the mid-crustal magma chamber (6.58 ± 0.46 RA) and fumaroles (7.31 ± 0.24 RA) of Oldoinyo Lengai attests that helium is not subjected to atmospheric contamination or crustal assimilation during transport to the surface.

Voir en ligne : http://dx.doi.org/10.1016/j.chemgeo...




publié vendredi 20 avril 2018