Yx. Zhu et al., SEDIMENTOLOGIC EVIDENCE FOR DATE OF SOUTHWARD MOVING OF THE YANGTZE-RIVER IN THE JIANGHAN PLAIN SINCE THE HOLOCENE, Chinese Science Bulletin, 43(8), 1998, pp. 659-662
The study of the sediment of Core M1 from Jianghan Plain suggests that
the sediment source of this area changed in the Holocene, which corre
sponds with the south moving of the Yangtze River. Since then, the sed
iment source has been mainly from the Hanshui River.