摘要
Multiphase solid inclusions within cumulus silicates, particularly olivine, in Fe-Ti oxide ores from the Lower Zone of the Baima intrusion, Emeishan large igneous province, SW China, have been identified for the first time using 2-D scanning electron microscope and 3-D high- resolution X-ray computed tomography.
Multiphase solid inclusions within cumulus silicates, particularly olivine, in Fe-Ti oxide ores from the Lower Zone of the Baima intrusion, Emeishan large igneous province, SW China, have been identified for the first time using 2-D scanning electron microscope and 3-D high- resolution X-ray computed tomography.
