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Kevin W. Burton

Researcher at Durham University

Publications -  152
Citations -  9825

Kevin W. Burton is an academic researcher from Durham University. The author has contributed to research in topics: Weathering & Stable isotope ratio. The author has an hindex of 55, co-authored 150 publications receiving 8667 citations. Previous affiliations of Kevin W. Burton include Centre national de la recherche scientifique & University of Michigan.

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Hf isotope ratio analysis using multi-collector inductively coupled plasma mass spectrometry: an evaluation of isobaric interference corrections

TL;DR: In this article, the correction of isobaric interferences involving accepted Yb isotope ratios and reasonable estimates of mass bias result in a significantly under-corrected 176Hf, which is proportional to the amount of Yb added.
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Ancient melt extraction from the oceanic upper mantle revealed by Re–Os isotopes in abyssal peridotites from the Mid-Atlantic ridge

TL;DR: In this paper, the major-, trace-element and rhenium-osmium (Re-Os) isotope data are presented for abyssal peridotites from Ocean Drilling Program (ODP) Leg 209, in the North Atlantic.
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Evolution of Nd and Pb isotopes in Central Pacific seawater from ferromanganese crusts

TL;DR: In this article, the authors used depth profiles of three Pacific ferromanganese crusts to obtain growth rates which are between 1.4 and 3.8 mm/Ma, indicating that eNd stratification in Pacific seawater, as demonstrated for the present day, has been maintained for at least 20 Ma.
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Molybdenum isotope evidence for global ocean anoxia coupled with perturbations to the carbon cycle during the Early Jurassic

TL;DR: In this paper, changes in seawater molybdenum isotope ratios (a proxy for seawater anoxia) during the Toarcian (Early Jurassic) OAE define the onset and expansion of oxygen deficient conditions.
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The influence of weathering processes on riverine magnesium isotopes in a basaltic terrain

TL;DR: In this paper, the major-, trace-element and Mg isotope data for the dissolved load and suspended particulates of Icelandic rivers draining dominantly basaltic catchments, including both glacier-fed and direct-runoff rivers, were analyzed.