Late Pleistocene and Holocene palaeoflood events recorded by slackwater deposits in the upper Hanjiang River valley, China
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文摘

Four episodes of palaeoflood events were identified in the upper Hanjiang River.

Flood peak discharges were estimated to 42,200–63,400 m3/s using hydraulic model.

These events occurred at 12,600–12,400, 4200–4000, 3200–2800 and 1900–1700 a BP.

These events represent a response of river system to monsoonal climatic variation.

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