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Economic Geology; November 1970; v. 65; no. 7; p. 856-861
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Relative concentrations of lattice defects as an index of the temperature of formation of fluorite

David J. McDougall

Thermoluminescence proportional to total number of defects, difference in dislocations (at or near equilibrium with existing thermal environment) and Frenkel imperfections (in metastable state and reflecting temperature of formation)

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