Diamond Fluorescence (فلورسنس الألماس) and the Geological History of Natural Diamond
Main Research Question
Can the type, intensity, and spatial distribution of fluorescence-related defect centers (مراكز العيوب) preserve information about diamond growth, mantle residence (الوشاح الأرضي), thermal history, and geological origin?
Fluorescence in diamond arises from optically active defect centres formed and modified during crystal growth, mantle residence, plastic deformation, and post-growth annealing. This project examines whether those centres carry a readable record of that history.
The scope is limited to natural, untreated diamond. Treated and laboratory-grown material is used only as a comparative control set.



