Physics
Scientist
Department of Earth Sciences, Oxford University, Parks Road, Oxford, OX1 3PR, UK
Department of Earth Sciences, University of Oxford, Parks Road, Oxford OX1 3PR, UK
Géosciences Marines, IFREMER, France
Department of Earth Sciences, Oxford University, UK
University of Oxford, Department of Earth Science, Parks Road, Oxford OX1 3PR, UK
Department of Earth Sciences, University of Oxford, UK
Department of Earth Sciences, University of Oxford, Oxford OX1 3PR, UK
Department of Earth Sciences, University of Oxford, Parks Road, Oxford OX2 6EH, UK
Department of Earth Sciences, University of Oxford, Parks Road, Oxford, OX2 6EH, UK
Department of Earth Sciences, Parks Road, Oxford OX1 3PR, UK
Lamont-Doherty Earth Observatory of Columbia University, Route 9W, 10964, Palisades, NY, USA
Department of Earth Sciences, University of Oxford, Parks Rd Oxford, OX1 3PR, England UK
Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK
Lamont-Doherty Earth Observatory of Columbia University, Route 9W, Palisades, NY, USA
Space Science and Applications, Los Alamos National Laboratory, Los Alamos, New Mexico, USA
Los Alamos National Laboratory, Los Alamos, New Mexico, NM, USA
Los Alamos National Laboratory, NIS-1, MS D466, Los Alamos, NM 87545, USA
Los Alamos National Laboratory, ISR-1 MS D466, Los Alamos, NM 87545, USA
Los Alamos National Laboratory, MS D466, Los Alamos, NM 87545, USA
Los Alamos National Laboratory, Mail Stop D466, Los Alamos, NM 87545, USA
TA-3 Building 040 Room S110A
ISR-1, Space and Atmospheric Sciences, Los Alamos National Laboratory, P.O. Box 1663, MS D466, Los Alamos, NM 87545, USA
Space and Atmospheric Sciences Group, Los Alamos National Laboratory, Los Alamos, New Mexico, USA
LANL, MS D466, Los Alamos, NM, USA
Los Alamos National Laboratory, MS D466, Los Alamos, NM 87545, USA Alamos National Laboratory, Los Alamos, New Mexico
231Pa / 230Th fractionation by ocean transport, biogenic particle flux and particle type
231Pa/230Th as a paleocirculation proxy outside the North Atlantic
231Pa/230Th in the Argentine Basin as a tracer of past southern-source water-mass flow
234 U/ 238 U ratios in quaternary planktonic foraminifera
234U/238U ratios and 230Th ages for Hateruma Atoll corals: implications for coral diagenesis and seawater 234U/238U ratios
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