Original language | English |
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Pages (from-to) | 174-175 |
Journal | Terra Abstracts |
Volume | 11 |
Publication status | Published - 1999 |
Variation in the main detrital clay input at the 6-5 transition in the N. Atlantic ocean revealed by Nd-Sr-Pb isotope study of clay particles.
V. Bout-Roumazeilles, G.R. Davies, L. Labeyrie
Research output: Contribution to Journal › Meeting Abstract › Other research output