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High-pressure partial melting of garnet pyroxenite: possi... | ResearchHub
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High-pressure partial melting of garnet pyroxenite: possible mafic lithologies in the source of ocean island basalts
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Authors
Tetsu Kogiso
2 more
Tetsu Kogiso
•
M. Hirschmann
•
D. Frost
Published
November 8, 2003
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Journal
Earth and Planetary Science Letters
Topics
Materials Science
Paleontology
Geophysics
Geochemistry
Composite Material
Show all topics
DOI
10.1016/s0012-821x(03)00538-7
