Sulphur isotopes of alkaline magmas unlock long-term records of crustal recycling on Earth

William Hutchison (), Rainer J. Babiel, Adrian A. Finch, Michael A. W. Marks, Gregor Markl, Adrian J. Boyce, Eva E. Stüeken, Henrik Friis, Anouk M. Borst and Nicola J. Horsburgh
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William Hutchison: University of St Andrews
Rainer J. Babiel: Mathematisch-Naturwissenschaftliche Fakultät, FB Geowissenschaften, Universität Tübingen
Adrian A. Finch: University of St Andrews
Michael A. W. Marks: Mathematisch-Naturwissenschaftliche Fakultät, FB Geowissenschaften, Universität Tübingen
Gregor Markl: Mathematisch-Naturwissenschaftliche Fakultät, FB Geowissenschaften, Universität Tübingen
Adrian J. Boyce: Scottish Universities Environmental Research Centre
Eva E. Stüeken: University of St Andrews
Henrik Friis: University of Oslo
Anouk M. Borst: University of St Andrews
Nicola J. Horsburgh: University of St Andrews

Nature Communications, 2019, vol. 10, issue 1, 1-12

Abstract: Abstract Earth’s surface and mantle sulphur reservoirs are connected via subduction, crustal recycling and volcanism. Although oceanic hotspot lavas currently provide the best constraints on the deep sulphur cycle, their restricted age range (

Date: 2019
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DOI: 10.1038/s41467-019-12218-1

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