Formation of ultra-depleted mantle peridotites and their relationship with boninitic melts: an example from the Kamuikotan Unit, Hokkaido, Japan

<p>Additional Supporting Information</p> <p>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</p> <p>QGIS<br> Geological map of the studied area</p>