Article ID Journal Published Year Pages File Type
5401039 Journal of Luminescence 2012 7 Pages PDF
Abstract
Cathodoluminescence (CL) of laboratory forsterite chondrules has been characterized to clarify the formation process of chondrules and related mechanism of the crystal growth in a supercooled melt. Color CL image of the experimentally grown forsterite exhibits significant blue luminescence in the main branches of the interior structure of lab-chondrule, which reflects to the anisotropy of crystallization. A new CL band centered at 450-525 nm (2.76-2.36 eV) in blue to green region might be assigned to a microdefect-related center, which is a diagnostic peak for the forsterite that was formed due to the rapid growth as high as ∼10 mm/s or higher from a supercooled melt.
Related Topics
Physical Sciences and Engineering Chemistry Physical and Theoretical Chemistry
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