Melt-mantle interactions beneath the Kamchatka arc: Evidence from ultramafic xenoliths from Shiveluch volcano-Reference-Cited by-同舟云学术

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Melt-mantle interactions beneath the Kamchatka arc: Evidence from ultramafic xenoliths from Shiveluch volcano

Published:2007-04 Issue:4 Volume:8 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Bryant J. A.¹,Yogodzinski G. M.¹,Churikova T. G.²

Affiliation:

1. Department of Geological Sciences; University of South Carolina; 701 Sumter Street,; Columbia; South Carolina; 29208; USA

2. Institute of Volcanology and Seismology Far East Division; Russian Academy of Sciences; 9 Piip Avenue,; Petropavlovsk-Kamchatsky; 683006; Russia

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference87 articles.

1. Three-dimensional flow and reaction in porous media: Implications for the Earth's mantle and sedimentary basins;Aharonov;J. Geophys. Res.,1997

2. Characterization of spinel peridotites by olivine-spinel compositional relationships: Review and interpretation;Arai;Chem. Geol.,1994

3. Origin of fine-grained peridotite xenoliths from Iraya volcano of Batan Island, Philippines: Deserpentinization or metasomatism at the wedge mantle beneath an incipient arc?;Arai;Island Arc,2000

4. Metasomatized harzburgite xenoliths from Avacha volcano as fragments of mantle wedge of the Kamchatka arc: Implications for the metasomatic agent;Arai;Island Arc,2003

5. Petrology of peridotite xenoliths from Iraya Volcano, Philippines, and its implications for dynamic mantle-wedge processes;Arai;J. Petrol.,2004

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