日時 ： ２００８年５月９日（金）17：00〜
場所 ： 愛媛大学理学部講義棟 室
要 旨
Pyrolite has been considered to present the Earth's mantle composition. Therefore, detailed studies of the phase relations and mineral physics properties in pyrolite over a wide pressure and temperature condition are required in order to understand the mineralogy and dynamics of the entire mantle. Many experimental investigations for pyrolite have been performed so far, however, the pressure conditions are limited up to 30 GPa. In this study, we have conducted in situ X-ray diffraction experiments to clarify the phase relations, Fe-Mg partitioning and density changes in pyrolite under the lower mantle conditions by using a combination of a multianvil apparatus and synchrotron radiation.
問い合わせ先：土屋 卓久 TEL （089）927-8198
E-mail takut@sci.ehime-u.ac.jp
