Dunite channels within a harzburgite layer from the Horoman peridotite complex, Japan: Possible pathway for magmas
Author:
Affiliation:
1. Institute for Geothermal Sciences, Graduate School of Science; Kyoto University; Beppu 874-0903 Japan
2. Hokkaido University Museum; Sapporo 060-0810 Japan
3. School of Earth Sciences; University of Tasmania; Hobart Tasmania 7001 Australia
Funder
Japan Society for the Promotion of Science
Publisher
Wiley
Subject
Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/iar.12279/fullpdf
Reference73 articles.
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3. Characterization of spinel peridotites by olivine-spinel compositional relationships: Review and interpretation;Arai;Chemical Geology,1994
4. Formation and compositional variation of phlogopites in the Horoman peridotite complex, Hokkaido, northern implications for origin and fractionation of metasomatic fluids in the upper mantle;Arai;Contributions to Mineralogy and Petrology,1989
5. Podiform chromitites of the Tari-Misaka ultramafic complex, southwestern Japan, as mantle-melt interaction products;Arai;Economic Geology,1994
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