Nuclear georeactor origin of oceanic basalt 3He/4He, evidence, and implications
Nuclear georeactor origin of oceanic basalt 3He/4He, evidence, and implications
复制标题
海洋玄武岩 3He/4He 的核地质反应器起源、证据和意义
DOI：
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复制
发表时间：
2003
影响因子：
11.1
通讯作者：
J. Herndon
中科院分区：
文献类型：
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作者：
J. Herndon
Nuclear georeactor numerical simulation results yield substantial 3He and 4He production and 3He/4He ratios relative to air (RA) that encompass the entire 2-SD (2σ) confidence level range of tabulated measured 3He/4He ratios of basalts from along the global spreading ridge system. Georeactor-produced 3He/4He ratios are related to the extent of actinide fuel consumption at time of production and are high near the end of the georeactor lifetime. Georeactor numerical simulation results and the observed high 3He/4He ratios measured in Icelandic and Hawaiian oceanic basalts indicate that the demise of the georeactor is approaching. Within the present level of uncertainty, one cannot say precisely when georeactor demise will occur, whether in the next century, in a million years, or in a billion years from now.
