Abundances of Uranium and Thorium Elements in Earth Estimated by Geoneutrino Spectroscopy

S. Abe,S. Asami,M. Eizuka,S. Futagi, A. Gando,Y. Gando,T. Gima,A. Goto,T. Hachiya,K. Hata,K. Hosokawa,K. Ichimura,S. Ieki,H. Ikeda,K. Inoue,K. Ishidoshiro,Y. Kamei,N. Kawada,Y. Kishimoto,M. Koga,M. Kurasawa,N. Maemura,T. Mitsui,H. Miyake,T. Nakahata,K. Nakamura,R. Nakamura,H. Ozaki,T. Sakai,H. Sambonsugi,I. Shimizu,Y. Shirahata,J. Shirai,K. Shiraishi, A. Suzuki,Y. Suzuki,A. Takeuchi,K. Tamae,H. Watanabe,Y. Yoshida,S. Obara,A. K. Ichikawa,S. Yoshida,S. Umehara,K. Fushimi,K. Kotera,Y. Urano,B. E. Berger,B. K. Fujikawa,J. G. Learned,J. Maricic,S. N. Axani,Z. Fu,J. Smolsky,L. A. Winslow,Y. Efremenko,H. J. Karwowski,D. M. Markoff, W. Tornow,A. Li,J. A. Detwiler,S. Enomoto,M. P. Decowski,C. Grant,H. Song,T. O'Donnell,S. Dell'Oro

Geophysical research letters（2022）

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关键词
geoneutrino,radiogenic heat,Earth's interior,mantle composition
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