title: 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.
authors.forename: M I
authors.initials: MI
authors.lastname: Petaev
authors.forename: A J
authors.initials: AJ
authors.lastname: Brearley