Gamma-Ray Spectrometry as a Tool for a Rapid Investigation of Detritic Cores
1969
ABSTRACT The nondestructive gamma-ray spectrometry of a sedimentary core allowed us to distinguish five great zones of variation for potassium and thorium content. A sedimentological and paleoclimatic study shows that those variations correspond to climatic fluctuations. It is then concluded that non destructive gamma-ray spectrometry may be a valuable tool for a rapid investigation of sedimentary cores.
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