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Showing 1 to 2 of 2 for “"non traditional stable isotopes"”.
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Studies of Magmatism by Trace Element Partitioning Between Clinopyroxene and Silicate Melt, Uranium-Series Disequilibria in Lavas From Subduction Zones, and Non-Traditional Stable Isotopes
… conclude that the positive co-variation of Fe-Mg isotopes could be an important fingerprint of magma differentiation in a temperature gradient.
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Investigation of iron isotope variability in the bimodal Aztec Wash Pluton, Eldorado Mountains, Nevada
… an isotopic signature was also observed: heavy isotopes of Fe, Mg, O, H and Li became enriched in the cold, felsic end of the gradient (Bindeman, et al., 2013; Huang et al., 2009). This isotopic trend is strikingly similar to one found in igneous systems, in which non-traditional stable isotopes …