Exsolution in ferromagnesian olivine of the divnoe meteorite.

Abstract

Ferromagnesian olivine, one of the most common minerals in the solar system, has been widely regarded as a continuous solid solution, although several thermodynamic analyses have suggested the possibility of a miscibility gap at low temperatures. Natural ferromagnesian olivine from the Divnoe meteorite contains compositionally different exsolution lamellae, providing direct evidence for the existence of a miscibility gap in iron-magnesium olivine solid solutions.

Cite this paper

@article{Petaev1994ExsolutionIF, title={Exsolution in ferromagnesian olivine of the divnoe meteorite.}, author={Michail I. Petaev and Adrian . J . Brearley}, journal={Science}, year={1994}, volume={266 5190}, pages={1545-7} }