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Debret, B., Millet, M.-A., Pons, M.-L., Bouilhol, P., Inglis, E., Williams, H. (2016) Isotopic evidence for iron mobility during subduction. Geology, 44 (3) 215-218 doi:10.1130/g37565.1

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Reference TypeJournal (article/letter/editorial)
TitleIsotopic evidence for iron mobility during subduction
JournalGeology
AuthorsDebret, B.Author
Millet, M.-A.Author
Pons, M.-L.Author
Bouilhol, P.Author
Inglis, E.Author
Williams, H.Author
Year2016 (March)Volume44
Page(s)215-218Issue3
PublisherGeological Society of America
DOIdoi:10.1130/g37565.1Search in ResearchGate
Mindat Ref. ID142965Long-form Identifiermindat:1:5:142965:1
GUID8bee7a3d-af55-46d6-bf98-6298f4811a79
Full ReferenceDebret, B., Millet, M.-A., Pons, M.-L., Bouilhol, P., Inglis, E., Williams, H. (2016) Isotopic evidence for iron mobility during subduction. Geology, 44 (3) 215-218 doi:10.1130/g37565.1
Plain TextDebret, B., Millet, M.-A., Pons, M.-L., Bouilhol, P., Inglis, E., Williams, H. (2016) Isotopic evidence for iron mobility during subduction. Geology, 44 (3) 215-218 doi:10.1130/g37565.1
In(2016, March) Geology Vol. 44 (3) Geological Society of America

References Listed

These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.

Alt (2003) Sulfur geochemistry and reaction modeling: Geochimica et Cosmochimica Acta Serpentinization of abyssal peridotites from the MARK area, Mid-Atlantic Ridge 67, 641
Not Yet Imported: Treatise on Geochemistry - book-chapter : 10.1016/B978-0-08-095975-7.00204-7

If you would like this item imported into the Digital Library, please contact us quoting Journal ID
Debret (2013) A LA-ICPMS study of the Lanzo ultramafic massif (Western Alps): Chemical Geology Trace element behavior during serpentinization/deserpentinization of an eclogitized oceanic lithosphere 357, 117
Debret (2014) Implications for the nature of the fluid released at depth: Terra Nova F, Cl and S input via serpentinite in subduction zones 26, 96
Debret (2015) Contributions to Mineralogy and Petrology Redox state of iron during high-pressure serpentinite dehydration 169, 18
Deschamps (2010) Timing of serpentinization and behavior of fluid-mobile elements in subduction zones: Chemical Geology In situ characterization of serpentinites from forearc mantle wedges 269, 262
Ding (1992) Iron solubility constrains on pH of subseafloor hydrothermal fluids: Geochimica et Cosmochimica Acta Determination of Fe-Cl complexing in the low pressure supercritical region (NaCl fluid) 56, 3681
Hattori (2007) Geosystems Geochemical character of serpentinites associated with high- to ultrahigh-pressure metamorphic rocks in the Alps, Cuba, and the Himalayas: Recycling of elements in subduction zones: Geochemistry, Geophysics 8, Q09010
Lafay (2013) Example from the Piedmont zone of the western Alps: Chemical Geology High-pressure serpentinites, a trap-and-release system controlled by metamorphic conditions 343, 38
Mungall (2002) Slab melting and the genesis of major Au and Au-rich Cu deposits: Geology Roasting the mantle 30, 915
Rapp (2010) An experimental investigation: Geology Extremely high solubility of rutile in chloride and fluoride-bearing metamorphic fluids 38, 323
Williams (2005) The effects of partial melting and oxygen fugacity: Earth and Planetary Science Letters Systematic iron isotope variations in mantle rocks and minerals 235, 435


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