Abstract
The spatial distribution of ESR signal intensity and equivalent dose ( D E) has been predicted within the quartz grains from fault gouge by the localized lattice deformation and frictional heating theory (Lee and Schwarcz, 1994). The abrading technique was applied to a fault gouge sample in order to see the distribution as the technique removes the surface semi-quantitatively. Both intensities of E′ 1 and Al centers become larger after abrasion, being consistent with the theory, but not all the D ES.
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