Abstract
HELIUM isotope studies1,2 have identified the Banda arc section of the Indonesian archipelago as the only circum-Pacific volcanic arc with 3He/4He ratios significantly lower than the common ratio in mid-ocean-ridge basalts (MORB). In eleven of twelve circum-Pacific arcs, MORB-like 3He/4He ratios show that helium in these volcanic terrains is dominantly primordial helium from the mantle wedge above the sinking slab, rather than radiogenic helium from subducting oceanic crust or sediments. Only in the Banda arc have significantly lower ratios been observed, corresponding to as much as 80% radiogenic helium from subducting continental material2. We now report 3He/4He measurements along a 1,800-km section of the Sunda arc, a region of underthrust oceanic lithosphere, showing MORB-like ratios from western Java to a surprisingly sharp transition zone centred on Lomblen Island, where the low ratios of the Banda arc begin. Our results confirm the prediction2 that Sunda arc volcanoes should have MORB-like 3He/4He ratios, with a well-defined transition to the much lower Banda arc ratios near Lewotolo volcano, and demonstrate a remarkable linkage of helium isotope variations with tectonic processes not readily discernible with trace elements or other isotopes.
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Hilton, D., Craig, H. A helium isotope transect along the Indonesian archipelago. Nature 342, 906–908 (1989). https://doi.org/10.1038/342906a0
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DOI: https://doi.org/10.1038/342906a0
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