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Helium isotopes as geochemical indicators of a serpentinized fore-arc mantle wedge

Umeda, Koji; McCrank, G. F.*; Ninomiya, Atsushi

New helium isotope data from hot springs on the eastern Kyushu Island were obtained from a large number of sampling points in order to elucidate the geographical distribution of $$^{3}$$He/$$^{4}$$He ratios in the fore-arc regions of Southwest Japan. Systematic, regional variations in $$^{3}$$He/$$^{4}$$He ratios can be identified clearly on between Kyushu Island (0.093-0.79 R$$_{rm A}$$), Shikoku Island (0.21-2.5 R$$_{rm A}$$) and the Kii Peninsula (0.39-7.4 R$$_{rm A}$$). The overall distribution of relative mantle helium reveals a close association with the occurrence of non-volcanic deep low-frequency tremors (LFT), which would be related to the presence of upward aqueous fluids produced by slab dehydration, in Southwest Japan. A flux of $$^{3}$$He carried by aqueous fluids via the mantle wedge is very low in Kyushu Island where the LFT are not found, resulting in a $$^{3}$$He/$$^{4}$$He ratio lower than the atmospheric ratio.

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Category:Geochemistry & Geophysics

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