Original paper

In situ X-ray study of perovskite (MgSiO3): Phase transition and dissociation at mantle conditions

Saxena, Surendra K.; Dubrovinsky, Leonid S.; Lazor, Peter; Hu, Jingzhu

European Journal of Mineralogy Volume 10 Number 6 (1998), p. 1275 - 1282

12 references

published: Dec 1, 1998
manuscript accepted: Jun 15, 1998
manuscript received: Jan 12, 1998

DOI: 10.1127/ejm/10/6/1275

BibTeX file

ArtNo. ESP147051006013, Price: 29.00 €

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Abstract The dissociation reaction: MgSiO3 (perovskite) = MgO (periclase) + SiO2 (high pressure silica phase) was studied at 82 (3) GPa by in situ heating to temperatures between 300 and 1780 (50) K and X-ray diffraction. The orthorhombic perovskite changed to a pseudo-cubic phase between 1280 to 1485 K followed by a break down to the oxide mixture which was observed to grow at temperatures between 1600 to 1700 K; orthorhombic perovskite was recovered upon cooling at 1140 K. In yet another experiment, MgO and the silica phase grew from a sample of enstatite composition at 82 GPa and 1250 K. Compositionally, the instability of perovskite makes the oxide mixture as the most probable mantle material which can provide a variety of possible mantle compositions. Dynamically, the lighter SiO2 component would facilitate differentiation of the lower mantle