Chemical interactions in the subduction factory: New insights from an in situ trace element and hydrogen study of the Ichinomegata and Oki-Dogo mantle xenoliths (Japan)

Author:

Satsukawa Takako,Godard Marguerite,Demouchy Sylvie,Michibayashi Katsuyoshi,Ildefonse Benoit

Funder

Scientific Research as part of a JSPS Research Fellowship for Young Scientists

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference192 articles.

1. Hydration processes in the arc mantle; petrology of the Megata peridotite xenoliths, the Northeast Japan arc;Abe;J. Mineral., Petrol. Econ. Geol.,1992

2. Petrographical characteristics of ultramafic xenoliths from the Megata volcano, the Northeast Japan arc;Abe;Sci. Rep. Kanazawa Univ.,1993

3. Geochemical characteristics of the uppermost mantle beneath the Japan island arcs; implications for the upper mantle evolution;Abe;Phys. Earth Planet. Inter.,1998

4. Geochemistry of the ultramafic xenoliths from Oki-Dogo island: implications for the wedge mantle evolution;Abe;Ofioliti,1999

5. Abe, N., Hirai, H., Arai, S., O'Reilly, S.Y., 2002. Geochemical signatures of high-T mantle xenoliths from Noyamadake, SW Japan: Implications from trace-element characteristics, Fourth International Workshop on Orogenic Lherzolite and Mantle Processes, Samani, Hokkaido, Japan.

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