%0 Journal Article
%T Sequences and Genesis of Yellow River Terrace from Sanmen Gorge to Kouma<br>黄河三门峡至扣马段的阶地序列及成因
%A SU Huai
%A WANG Junping
%A PAN Baotian
%A MING Qingzhong
%A SHI Zhengtao
%A <br>苏怀
%A 王均平
%A 潘保田
%A 明庆忠
%A 史正涛
%J 地理学报
%D 2008
%I 
%X Based on field and geomorphologic investigations,along with analysis of thermoluminescence(TL),magnetostratigraphy and loess-paleosol sequence on terraces,we found that at least four Yellow River terraces,whose ages are 0.86 Ma,0.62 Ma,0.13 Ma and 0.05 Ma,have been developed on west Henan fault-uplift system from Sanmen Gorge to Mengjin reach and but only three Yellow River terraces,whose ages are 1.24 Ma,0.25 Ma and 0.05 Ma,have been developed on North China fault depression system from Mengjin to Kouma reach.All the terraces have similar structure that they have paleosols with a thickness of several meters developed on top of the fluvial silt.It shows that the Yellow River incised when terraces were abandoned during the transitional period from glacial to interglacial and there may be a link between the formation of terraces and glacial-interglacial climatic cycles.However,the differences in Yellow River terrace sequences between the two tectonic units,i.e.,west Henan fault-uplift and North China fault depression,indicate that the land uplift has been playing an important role in the formation of these terraces.
%K Sanmen Gorge
%K Yellow River terrace
%K climatic change
%K land uplift<br>三门峡
%K 黄河阶地
%K 气候变化
%K 地面抬升
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=869B153A4C6B5B85&jid=F7B5B947C24B9D649491012214E4BEF4&aid=A9D4FEB5B9935BF2F91ABC2C993B891E&yid=67289AFF6305E306&vid=E84BBBDDD74F497C&iid=DF92D298D3FF1E6E&sid=195767709E606C85&eid=626A0FE8E3130AB5&journal_id=0375-5444&journal_name=地理学报&referenced_num=2&reference_num=28