Molybdenum isotope composition of the upper mantle and its origin: insight from mid-ocean ridge basalt
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Springer Science and Business Media LLC
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https://link.springer.com/content/pdf/10.1007/s00343-024-3250-6.pdf
Reference15 articles.
1. Bezard R, Fischer-Gödde M, Hamelin C et al. 2016. The effects of magmatic processes and crustal recycling on the molybdenum stable isotopic composition of Mid-Ocean Ridge Basalts. Earth and Planetary Science Letters, 453: 171–181, https://doi.org/10.1016/j.epsl.2016.07.056.
2. Burkhardt C, Hin R C, Kleine T et al. 2014. Evidence for Mo isotope fractionation in the solar nebula and during planetary differentiation. Earth and Planetary Science Letters, 391: 201–211, https://doi.org/10.1016/j.epsl.2014.01.037.
3. Chen S, Hin R C, John T et al. 2019. Molybdenum systematics of subducted crust record reactive fluid flow from underlying slab serpentine dehydration. Nature Communications, 10(1): 4773, https://doi.org/10.1038/s41467-019-12696-3.
4. Chen S, Sun P, Niu Y L et al. 2022. Molybdenum isotope systematics of lavas from the East Pacific Rise: constraints on the source of enriched mid-ocean ridge basalt. Earth and Planetary Science Letters, 578: 117283, https://doi.org/10.1016/j.epsl.2021.117283.
5. Freymuth H, Vils F, Willbold M et al. 2015. Molybdenum mobility and isotopic fractionation during subduction at the Mariana arc. Earth and Planetary Science Letters, 432: 176–186, https://doi.org/10.1016/j.epsl.2015.10.006.
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