Exsolution in Ferromagnesian Olivine of the Divnoe Meteorite

Details Exsolution in Ferromagnesian Olivine of the Divnoe Meteorite Exsolution in Ferromagnesian Olivine of the Divnoe Meteorite

Dec 1994

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1994sci...266.1545p&link_type=abstract

Science, Volume 266, Issue 5190, pp. 1545-1547

Computer Science

5

Scientific paper

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.

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