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Mantle Plumes Originate from 670 km Depth: Implications of Phase Relations on Mantle Peridotite at 20-25 GPa and 1700-2200 degrees C (abs.)
TAKAHASHI Eiichi
itemdescription
TitleMantle Plumes Originate from 670 km Depth: Implications of Phase Relations on Mantle Peridotite at 20-25 GPa and 1700-2200 degrees C (abs.)
AuthorsTAKAHASHI Eiichi
Data nameEOS, Transactions, American Geophysical Union, 1997 Fall Meeting
Volume78
Num46 suppl.
PageF11-F11
Year1997
PublisherAmerican Geophysical Union
LanguageEN
ISSN00963941
@idhttps://gbank.gsj.jp/ld/resource/geolis/199708261