A mixture of graphite and Fe2SiO4 in a ratio 2:3 by weight has been studied
under pressures from 6 to 10 GPa and temperatures between 1000 and 1960 de
grees C using an octahedral-anvil apparatus. At 8 GPa, diamond with a size
similar to 10 mu m across was found to be formed at temperatures higher tha
n 1900 degrees C. This threshold temperature is by 150 degrees C higher tha
n the melting temperature of Fe2SiO4 at this pressure. The result offers a
clue to the genesis of diamond in the deep interior of the earth.