Once subducted into the mantle, material from Earth's continental crust seems to disappear. But its distinctive isotopic signature has been found back at the surface — in volcanic rocks on a Pacific island.
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References
Widom, E. Nature 443, 516–517 (2006).
Jackson, M. G. et al. Nature 448, 684–687 (2007).
White, W. M. & Hofmann, A. W. Nature 296, 821–825 (1982).
Workman, R. K. et al. Geochem. Geophys. Geosyst. 5, doi:10.1029/2003GC000623 (2004).
Hofmann, A. W., Jochum, K. P., Seufert, M. & White, W. M. Earth Planet. Sci. Lett. 79, 33–45 (1986).
Zindler, A. & Hart, S. R. Annu. Rev. Earth Planet. Sci. 14, 493–571 (1986).
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Hofmann, A. The lost continents. Nature 448, 655–656 (2007). https://doi.org/10.1038/448655a
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DOI: https://doi.org/10.1038/448655a
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