Heat-producing Elements
Heat-Producing Elements is a geochemical construct denoting a class of radioactive isotopes, primarily uranium, thorium, and potassium-40, whose intrinsic property of spontaneous decay generates thermal energy within planetary interiors, thereby fundamentally influencing the thermal evolution of terrestrial bodies.
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2017–2026
49
Variants
Heat-producing IsotopesHpe
Parents
213
Urey ratio and the structure and evolution of Earth's mantle
Jun Korenaga · Reviews of Geophysics · 2008 · 371 citations
Age and composition of young basalts on the Moon, measured from samples returned by Chang’e-5
Xiaochao Che, A. A. Nemchin, Dunyi Liu et al. · Science · 2021 · 340 citations · Full text
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Rutgers, The State University of New Jersey, United States
3 publications · 185 citations
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Centre National de la Recherche Scientifique
Paris, France
10 h-index
38 publications
4.3K citations
Université Paris Cité
Paris, France
7 h-index
24 publications
2.2K citations
Purdue University West Lafayette
West Lafayette, United States
7 h-index
12 publications
586 citations
ETH Zurich
Zurich, Switzerland
7 h-index
12 publications
2.5K citations

Australian National University
Canberra, Australia
7 h-index
10 publications
1.1K citations

Institut de physique du globe de Paris
Paris, France
6 h-index
22 publications
2.1K citations
Planetary Science Institute
Tucson, United States
6 h-index
9 publications
1K citations
University of Maryland, College Park
College Park, United States
6 h-index
13 publications
1.2K citations
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17 publications · 901 citations
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14 publications · 2.2K citations
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JGR · 8 publications · 885 citations
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7 publications · 958 citations
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