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

Name: Formation of ultra-depleted mantle peridotites and their relationship with boninitic melts: an example from the Kamuikotan Unit, Hokkaido, Japan
Creator: Arai, S.; Morishita, T; Szilas, K.; Tamura, A.; Itano, K.; Ichiyama, Y.; Nishio, I.; Takamizawa, S.; Barrett, N.
Published: 2022-10-29T00:00:00+08:00

Zenodo2022-10-29 更新2026-04-07 收录

橄榄石地球化学

玻安质熔体成因

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资源简介：

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

提供机构：

Arai, S.; Morishita, T; Szilas, K.; Tamura, A.; Itano, K.; Ichiyama, Y.; Nishio, I.; Takamizawa, S.; Barrett, N.

创建时间：

2022-10-29