Computer Science
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Department of Earth Sciences, The Open University, Walton Hall, MK7 6AA, Milton Keynes, UK
GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney, New South Wales 2109, Australia
Department of Earth Sciences, The Open University, Milton Keynes MK7 6AA, United Kingdom; Laboratoire de Tectonophysique, Centre National de la Recherche Scientifique-Institut des Sciences de la Terre, de l'Environnment, et de l'Espace de Montpellier, Université de Montpellier II, 34095 Montpellier, France; and
Department of Earth Sciences, The Open University, Walton Hall, Milton Keynes, MK7 6AA, UK
Geosciences Montpellier, Univ. Montpellier 2 - CNRS Place Eugene Bataillon, Montpellier, 34095 France
Géosciences Montpellier, Université de Montpellier 2 and CNRS, Cc 060, Place E. Bataillon, 34095 Montpellier cedex 5, France
GEMOC ARC National Key Centre, Department of Earth and Planetary Sciences, Macquarie University, NSW 2109, Australia; CNRS, Université de Montpellier, 34095 Montpellier, Cedex 05, France
GEMOC ARC National Key Centre, Department of Earth and Planetary Sciences, Macquarie University, Sydney, NSW 2109, Australia
GEMOC, Department of Earth Sciences, Macquarie University, Sydney, Australia
Department of Earth Science, The Open University, Walton Hall, Milton Keynes, MK7 6AA, UK; Geosciences Montpellier, Université Montpellier II, Place E. Bataillon, 34095, Montpellier cedex 05, France
Géosciences Montpellier, Université Montpellier II, CNRS, Place Eugène Bataillon 34095 Montpellier cedex 5, France
Ancient melt extraction from the oceanic upper mantle revealed by Re Os isotopes in abyssal peridotites from the Mid-Atlantic ridge
Geochemistry of the highly depleted peridotites drilled at ODP Sites 1272 and 1274 (Fifteen-Twenty Fracture Zone, Mid-Atlantic Ridge): Implications for mantle dynamics beneath a slow spreading ridge
Highly siderophile element behaviour accompanying subduction of oceanic crust: Whole rock and mineral-scale insights from a high-pressure terrain
Highly Siderophile Elements in Mantle Sulfides: In Situ Laser Ablation Microprobe Inductively Coupled Plasma Mass Spectrometry Analysis
How primitive is the "primitive" mantle?
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