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• W2013207924 abstract "New helium isotope data ( 3 He/ 4 He) from a series of co-genetic Siberian lavas of Cenozoic age (0.6 - 3 Ma) provide possible evidence for mass-dependent helium isotope fractionation. These lavas, erupted around the Baikal rift, have sampled subcontinental lithospheric mantle (SCLM). 3 He/ 4 He ratios measured in clinopyroxene and olivine phenocrysts are between 0.9 - 8.3 R a . The SCLM in this region is therefore characterised by the higher unmodified 3 He/ 4 He ratios, which are similar to the source region of mid-ocean ridge basalts (MORB). Helium isotope variation of this scale and order within local regional volcanic settings has previously been ascribed to purely, crustal contamination or radiogenic ingrowth of 4 He. However, we argue that helium isotopes may also be affected by mass-dependent fractionation. This can occur during helium diffusion from the phenocrysts within sub-solidus magmas." @default.
• W2013207924 created "2016-06-24" @default.
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• W2013207924 date "2004-03-29" @default.
• W2013207924 modified "2023-10-16" @default.
• W2013207924 title "Possible diffusive fractionation of helium isotopes in olivine and clinopyroxene phenocrysts" @default.
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• W2013207924 doi "https://doi.org/10.1127/0935-1221/2004/0016-0213" @default.
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