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V. R. Murthy 《Earth, Moon, and Planets》2006,99(1-4):23-32
The radioactivity of the earth is an important parameter in understanding the dynamics of the planet and the evolution of
the crust–mantle–core system but geochemical and geophysical approaches have had only a limited success in defining it. The
opportunity of a direct estimate of the radioactivity of the earth by measurement of the geoneutrino flux takes on an added
significance in this context. Such an independent new measurement will help resolve and/or clarify a number of questions about
global scale processes in the earth and will help advance earth sciences. 相似文献