Author Correction: Fossilized Melts in Mantle Wedge Peridotites.

An amendment to this paper has been published and can be accessed via a link at the top of the paper.

Fossilized Melts in Mantle Wedge Peridotites.

The shallow oxidized asthenosphere may contain a small fraction of potassic silicate melts that are enriched in incompatible trace elements and volatiles. Here, to determine the chemical composition of such melt, we analysed fossilized melt inclusions, preserved as multiphase solid inclusions, from an orogenic garnet peridotite in the Bohemian Massif. Garnet-poor (2 vol.