Partial melting process in the upper mantle deduced from morphological and chemical variations of the chromian spinel two-pyroxene symplectite due to progressive partial melting of the Horoman peridotite, Hokkaido, Japan
Released on J-STAGE: January 17, 2007 |
Volume 90
Issue 3
Pages 93-102
Tomoaki MORISHITA, Shoji ARAI, Natsuko TAKAHASHI