The behavior of iron and zinc stable isotopes accompanying the subduction of mafic oceanic crust: A case study from Western Alpine ophiolites

Author:

Inglis Edward C.1ORCID,Debret Baptiste12,Burton Kevin W.1,Millet Marc-Alban13ORCID,Pons Marie-Laure12,Dale Christopher W.1ORCID,Bouilhol Pierre14ORCID,Cooper Matthew5ORCID,Nowell Geoff M.1,McCoy-West Alex J.1ORCID,Williams Helen M.12

Affiliation:

1. Department of Earth Sciences, Science Labs; Durham University; Durham UK

2. Department of Earth Sciences; University of Cambridge; Cambridge UK

3. School of Earth and Ocean Science; Cardiff University; Cardiff UK

4. Université Clermont Auvergne, CNRS, IRD, OPGC, Laboratoire Magmas et Volcans; Clermont-Ferrand France

5. Ocean and Earth Science, National Oceanography Centre Southampton; University of Southampton; Southampton UK

Funder

European Research Council

NERC Deep Volatiles Consortium

Durham University International Junior Fellowship

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference113 articles.

1. The Zermatt-Saas ophiolite: The largest (60-km wide) and deepest (c. 70-80 km) continuous slice of oceanic lithosphere detached from a subduction zone?;Angiboust;Terra Nova,2009

2. Iron isotope constraints on Fe cycling and mass balance in oxygenated Earth oceans;Beard;Geology,2003

3. Where did Gustav Steinmann see the trinity? Back to the roots of an Alpine ophiolite concept;Bernoulli;Geol. Soc. Am. Spec. Pap.,2003

4. Calculation of equilibrium stable isotope partition function ratios for aqueous zinc complexes and metallic zinc;Black;Geochim. Cosmochim. Acta,2011

5. A numerical approach to melting in warm subduction zones;Bouilhol;Earth Planet. Sci. Lett.,2015

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