%0 Journal Article
%T Sedimentologic evidence for date of southward moving of the Yangtze River in the Jianghan Plain since the Holocene
%A Yuxin Zhu
%A Sumin Wang
%A Ruijin Wu
%A
%J 科学通报(英文版)
%D 1998
%I
%X The study of the sediment of Core M1 from Jianghan Plain suggests that the sediment source of this area changed in the Holocene, which corresponds with thr south moving of the Yangtze River. Since then, the sediment source has been mainly from the Hanshui River.
%K southword moving of the Yangtm River
%K dating
%K sedimentologic evidence
%K Holocene
%K the Jlanghan Plain
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=01BA20E8BA813E1908F3698710BBFEFEE816345F465FEBA5&cid=96E6E851B5104576C2DD9FC1FBCB69EF&jid=DD6615BC9D2CFCE0B6F945E8D5314523&aid=0D1A93785DF6B36D6B68546EEEE877E5&yid=8CAA3A429E3EA654&vid=BE33CC7147FEFCA4&iid=5D311CA918CA9A03&sid=00520952CD4BF212&eid=00520952CD4BF212&journal_id=1001-6538&journal_name=科学通报(英文版)&referenced_num=0&reference_num=9