Abstract
In part 1 of this paper a split sphere multipiston assemblage is introduced with which it is possible to produce ultra high pressure and temperature for synthetic experiments. The second part of this paper reports a study on high pressure and temperature stability relation in Mg-rich mineral olivine, i.e. the most occurring mineral in the earth's mantle. Then, a phase diagram in the system Mg 2SiO 4 and Fe 2SiO 4 is shown together with some technical remarks.
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