Physics
Scientist
Department of Earth Sciences, University of Oxford, South Parks Road, Oxford, OX1 3AN, UK
231Pa/230Th in the Argentine Basin as a tracer of past southern-source water-mass flow
Combining seawater 232Th and 230Th concentrations to determine dust fluxes to the surface ocean
The timings of sea level change during the last glacial cycle, from U/Th dating of submerged corals: Results from IODP expedition 310 "Tahit sea level"
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