Radiogenic heat, even from a fairly deep-seated uranium orebody, could be measured.
即使铀矿体埋得足够深,它的放射成因热也能被测出。
Using data gathered from other sources on potassium-the other major element-they were able to estimate that radiogenic heat accounts for half of the heat produced by the Earth.
使用从其他来源收集到的钾(另一种主要元素)的数据,放射热估计能够占地球产生的热量的一半。
The radiogenic heat production rate in the upper crust decreased with the increasing depth. However, they were distributed uniformly within the depth scale of sedimentary basin.
岩石生热率在上地壳的分布是随深度的增加而减小的,但在沉积盆地的深度范围内几乎不变,其分布是均匀的,仅不同岩性的生热率差别较大。
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