The ESR spectra and ages of the fractured rocks along the Itoigawa-Shizuoka Tectonic Line, a major fault in Japan, were measured. The ESR signal intensities tend to become larger with decreasing distance from the fault boundary, because the radiation sensitivities of the ESR centres have increased by faulting. According to fracturing and heating experiments, when the radiation sensitivities of ESR centres have visibly increased, the signals may have been almost completely reset by faulting. As a result of the increase of radiation sensitivity, the error range of the TD values for incompletely reset ESR signals is comparatively large, whereas it is smaller in the case of completely reset signals. Therefore, by assessing the error range of TD values we can determine whether ESR signals were completely reset at the time of faulting.
Read full abstract