Hydrous peridotitic fragments of Earth’s mantle 660 km discontinuity sampled by a diamond - Nature Geoscience

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Hydrous peridotitic fragments of Earth’s mantle 660 km discontinuity sampled by a diamond - Nature Geoscience
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An ocean inside the Earth? Water is determined to be hundreds of kilometers down goetheuni NatureGeosci

This research was supported by a GIA Liddicoat Postdoctoral Research Fellowship to T.G. Sincere thanks to T. Moses from GIA for access to this sample; J. W. Valley and B. L. Dutrow for their support on GIA research program; E. Yazawa and C. Zhou from GIA for technical assistance; K. Moe from GIA for assistance with Raman data collection; J. I. Koivula, N. D. Renfro and J. Liao from GIA for photomicrography; U. D’Haenens-Johansson from GIA for sample selection; E. Smith, K. Smit and M. Y.

has received funding from the European Union’s Horizon 2020 Marie Skłodowska-Curie grant agreement no. 796755. D.N. acknowledges the ‘Rita Levi Montalcini’ programme of the Italian Ministry of University and Research. M.A. is supported by a European Research Council grant agreement no. 714936 TRUE DEPTHS. F.N. thanks the ERC Starting Grant no. 307322 and the Alexander von Humboldt Foundation. Sincere thanks to O. Navon for constructive comments.

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