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[HCG35-02] ESR and TL signals in quartz in the present river sediments along with the Kurove river
Keywords:river sediment, provenance, ESR, TL
The number of oxygen vacancies, higher in the upper reach, gets lower in the middle, and further higher in the lower reaches due to the inflow of the sediments originated from the younger and from the older bedrocks, respectively. The high temperature red to low temperature blue TL ratios, higher in the upper reach, gets lower in the middle and lower reaches due to the sediments having lower values. The change in the values along with the river flow is found to be explained by the inflow of the sediments originated from the bedrocks around the river.