Metal-saturated peridotite in the mantle wedge inferred from metal-bearing peridotite xenoliths from Avacha volcano, Kamchatka

Earth and Planetary Science Letters

Volumn 284, Issue 3-4, 2009, Pages 352-360

  Ishimaru, Satoko ^a   Arai, Shoji ^a,b   Shukuno, Hiroshi ^b  

^a KANAZAWA UNIVERSITY   (Japan)

^b JAPAN AGENCY FOR MARINE EARTH SCIENCE AND TECHNOLOGY   (Japan)

Author keywords

frontal arc; mantle wedge; metals; peridotite xenolith; reducing fluids

Indexed keywords

CHEMICAL EQUILIBRIUMS; FRONTAL ARC; HIGH OXIDATION STATE; INCLUSION TRAILS; KAMCHATKA; LITHOSPHERIC MANTLE; MANTLE WEDGE; PERIDOTITE XENOLITH; PERIDOTITE XENOLITHS; REDUCING FLUIDS; SERPENTINIZATION; SUB-ARC MANTLE;

CAVITY RESONATORS; FLUIDS; METALS; MINERALS; PETROGRAPHY; PHASE EQUILIBRIA; SILICATE MINERALS; SILICIDES; VOLCANOES;

METAL MELTING;

ARC-ARC COLLISION; FOREARC BASIN; MANTLE STRUCTURE; METAL; OXIDATION; PERIDOTITE; TECTONIC WEDGE; XENOLITH;

AVACHA VOLCANO; EURASIA; KAMCHATKA; RUSSIAN FEDERATION;

EID: 67650538930     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2009.04.042     Document Type: Article

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