Earth's core heat is generated by radioactive decay and primordial heat
Scientific consensus strongly supports the view that Earth's internal heat is sustained by a combination of primordial heat from accretion and radiogenic heat from the decay of radioactive isotopes.
The retrieved literature consistently supports the long-standing geoscientific understanding that Earth's internal heat budget is driven by a combination of primordial heat and radiogenic heat production (such as from uranium, thorium, and potassium).
L. Sammon, W. McDonough. Quantifying Earth's radiogenic heat budget. 2022. https://doi.org/10.1002/essoar.10510480.1
Paper 2 discusses Earth's internal heat budget driven by both primordial and radiogenic sources.
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Luo H, O'Rourke JG, Deng J. Radiogenic heating sustains long-lived volcanism and magnetic dynamos in super-Earths.. 2024. https://doi.org/10.1126/sciadv.ado7603
Paper 9 states that roughly half of the heat Earth loses is from radiogenic sources, alongside primordial heat contributions.
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