Alluvial sedimentary records in the North China Plain are essential in expanding flood
history and understanding hazard patterns in the Yellow River basin where inundation risk …

The study of Holocene paleoflood can remedy the limitation of modern flood monitoring
records in time and space, and more scientifically identify the flooding regulations and …

Objective Late Holocene sedimentary records along the abandoned channel areas contain
lots of paleoflood information in the lower Yellow River, which can help to extend extreme …

Slackwater deposits have been used as evidence for the magnitude and frequency of
palaeofloods which occurred prior to gauged and historical data sets, eg, Holocene extreme …

A set of paleoflood slack water deposit (SWD) beds was identified within slope clasts at the
Jinpingcun (JPC) site in the Jingyuan–Jingtai reaches of the upper Yellow River gorges …

Based on the principle that the present is the key to the past, detailed analyses, such as
AMS 14 C dating, grain size, component and morphology of heavy minerals, micro …

In this paper we propose a new super-comprehensive proxy that integrates the sedimentary
rhythm indicators of grain size, black carbon, anthropogenic elements, and pollen for the …

Palaeoflood slackwater deposits (SWDs) are the natural record of overbank flooding and are
often found within aeolian loess-soil profiles along the river valleys of the middle Yellow …

Palaeoflood slackwater deposits (SWDs), are the natural record of overbank flooding and
are often found within aeolian loess‐soil profiles along the river valleys of the middle Yellow …

Paleohydrological investigations were carried out in the Luoyang Basin along the Luohe
River in the middle reaches of the Yellow River basin. Three units of overbank flood deposits …