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Fig. 5. | Progress in Earth and Planetary Science

Fig. 5.

From: Provenance changes in fine detrital quartz in the inner shelf sediments of the East China Sea associated with shifts in the East Asian summer monsoon front during the last 6 kyrs

Fig. 5.

ad Comparison of the ESR signal intensity and CI of quartz in the fine silt fraction of MD06-3040 core sediments to those sediments from various parts of the modern Yangtze River drainage (Saito et al. 2017) for intervals 2 to 5 covering the last 6.0 kyr BP identified in this study. The circles represent the average values of the ESR signal intensity and CI of quartz during each individual interval

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