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The Spatial Distribution of ESR Signals in Fault Gouge Revealed by Abrading Technique

机译:磨蚀技术揭示断层泥中ESR信号的空间分布

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摘要

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
机译:通过局部晶格变形和摩擦加热理论(Lee and Schwarcz,1994),从断层泥中预测了石英颗粒内ESR信号强度和等效剂量(D_E)的空间分布。研磨技术应用于断层泥样品,以便在该技术半定量去除表面时看到其分布。磨蚀后,E'_1和Al中心的强度都变大,这与理论一致,但并非所有D_E

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