Formation of ultra-depleted mantle peridotites and their relationship with boninitic melts: an example from the Kamuikotan Unit, Hokkaido, Japan
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Additional Supporting Information table_S1.xlsx: Compilation of the ultra-depleted peridotites<br> table_S1.xlsx: Locations and mineral major and trace elements compositions of the Takadomari and Horokanai ultra-depleted peridotites<br> table_S3.xlsx: Mineral and melt trace elements compositions obtained by our melting models QGIS<br> Geological map of the studied area
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2022-10-29
