B, Sr and Pb isotope geochemistry of high-pressure Alpine metaperidotites monitors fluid-mediated element recycling during serpentinite dehydration in subduction mélange (Cima di Gagnone, Swiss Central Alps)

Tectonic mixing of slab- and mantle-derived materials at the interface between converging plates highly enhances fluid-mediated mass transfer from the slab to the overlying mantle. Subduction mélanges can provide information about the interaction among different slices accreted at plate interface do...

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Bibliographic Details
Published inGeochimica et cosmochimica acta Vol. 163; pp. 80 - 100
Main Authors Cannaò, E., Agostini, S., Scambelluri, M., Tonarini, S., Godard, M.
Format Journal Article
LanguageEnglish
Published Elsevier Ltd 15.08.2015
Elsevier
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