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  • Relative contributions to Earth’s total heat flux from the radioactive decay of isotopes versus primordial heat are debated. Measurements of geoneutrino particles emitted during radioactive decay in the Earth’s interior indicate that radiogenic isotopes contribute only about half of the total heat flux.

    • A. Gando
    • Y. Gando
    • M. P. Decowski
    Research
    Nature Geoscience
    Volume: 4, P: 647-651