Computer Science
Scientific paper
Mar 1968
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1968gecoa..32..347y&link_type=abstract
Geochimica et Cosmochimica Acta, vol. 32, Issue 3, pp.347-352
Computer Science
1
Scientific paper
The rate of oceanic sedimentation was determined by gamma-ray spectrometry. The method consists of following the decay of the ratio Io:Th as a function of the depth in the core of sediment by measuring the gamma-rays emitted from their descendants. The sedimentation rate of an Indian Ocean core was determined as 1.2 mm/1000 yr. This value is compatible with previous results obtained by the chemical separation method of the thorium isotopes.
Grjebine Tovy
Labeyrie Jacques
Tobailem Jacques
Yokoyama Yuji
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