The potential of Ca isotopes to trace subducted marine carbonates in deep mantle
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Springer Science and Business Media LLC
Link
https://link.springer.com/content/pdf/10.1007/s00343-024-4021-0.pdf
Reference64 articles.
1. Antonelli M A, Giuliani A, Wang Z et al. 2023. Subducted carbonates not required: deep mantle melting explains stable Ca isotopes in kimberlite magmas. Geochimica et Cosmochimica Acta, 348: 410–427, https://doi.org/10.1016/j.gca.2023.03.025.
2. Antonelli M A, Mittal T, McCarthy A et al. 2019a. Ca isotopes record rapid crystal growth in volcanic and subvolcanic systems. Proceedings of the National Academy of Sciences of the United States of America, 116(41): 20315–20321, https://doi.org/10.1073/pnas.1908921116.
3. Antonelli M A, Schiller M, Schauble E A et al. 2019b. Kinetic and equilibrium Ca isotope effects in high-T rocks and minerals. Earth and Planetary Science Letters, 517: 71–82, https://doi.org/10.1016/j.epsl.2019.04.013.
4. Antonelli M A, Simon J I. 2020. Calcium isotopes in high-temperature terrestrial processes. Chemical Geology, 548: 119651, https://doi.org/10.1016/j.chemgeo.2020.119651.
5. Banerjee A, Chakrabarti R. 2019. A geochemical and Nd, Sr and stable Ca isotopic study of carbonatites and associated silicate rocks from the ∼65 Ma old Ambadongar carbonatite complex and the Phenai Mata igneous complex, Gujarat, India: implications for crustal contamination, carbonate recycling, hydrothermal alteration and source-mantle mineralog. Lithos, 326–327: 572–585, https://doi.org/10.1016/j.lithos.2019.01.007.
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