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1 Introduction Geoneutrinos (electron antineutrinos from beta decays of Heat-Producing Elements, HPEs: K, Th, U) are a direct probe of the radioactive content of the deep Earth. Each decay releases an antineutrino-to-heat ratio fixed by nuclear physics, so the geoneutrino flux measured at the surface fixes the radiogenic heat budget when interpreted within a known geological framework (Bellini et al., 2021; Fiorentini et al., 2007).
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