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

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

doi:10.5281/zenodo.7263366

Published October 29, 2022 | Version v2

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

1. Kanazawa University
2. Akita University
3. Chiba University
4. University of Copenhagen

Additional Supporting Information

table_S1.xlsx: Compilation of the ultra-depleted peridotites
table_S1.xlsx: Locations and mineral major and trace elements compositions of the Takadomari and Horokanai ultra-depleted peridotites
table_S3.xlsx: Mineral and melt trace elements compositions obtained by our melting models

QGIS
Geological map of the studied area

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Created: October 29, 2022
Modified: October 30, 2022

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_Info_N2022_JGR.zip

Files (410.0 kB)