T. Yagi et al., POST-GARNET HIGH-PRESSURE TRANSITION - EFFECT OF HETEROGENEOUS LASER-HEATING AND INTRODUCTION OF SOME NEW TECHNIQUES, European journal of mineralogy, 9(2), 1997, pp. 301-310
The post-garnet high-pressure transition has been studied above 25 GPa
using several high-pressure apparatus. Recovered samples were charact
erized using SEM and TEM coupled with energy-dispersive electron-micro
probe analysis, and powder X-ray diffraction. Combined with the result
s of previous work, it became clear that, in the case of garnet, the r
esulting high-pressure phases differ considerably depending on the det
ails of the high-pressure experiments. The current study shows that he
terogeneous heating by YAG laser in the diamond anvil cell may be resp
onsible for some of the complexity of previous results. Much more unif
orm heating of the sample is now possible using a resistance furnace i
n a Drickamer-type apparatus or CO2-laser heating in a diamond-anvil c
ell. The results of the current experiments indicate that end-member p
yrope garnet transforms into a mixture of perovskite and corundum phas
es in the pressure range of about 30 GPa.