%0 Journal Article
%T THE DENUDATIONAL-SURFACE SEQUENCE AND CONTROLS ON THE LANDSCAPTE DEVELOPMENT IN THE LANGSHAN MOUNTAINS-SEERTENGSHAN MOUNTAINS,INNER MONGOLIA<br>内蒙古狼山-色尔腾山的剥蚀面序列 和景观发育的控制因素*
%A Cheng Shaoping
%A Li Chuanyou
%A Yang Guizhi
%A Ren Defeng
%A <br>程绍平
%A 李传友
%A 杨桂枝
%A 任德风
%J 第四纪研究
%D 2006
%I 
%X The denudational-surface sequence and its distribution pattern in the Langshan Mountains-Seertengshan Mountains on the northern flank of the Hetao Rift Zone,Inner Mongolia,have been defined in terms of numerical data associated with the present ground surface.The rifting that initiated at the end of Eocene has caused four regional surface uplifts and denudations in Oligocene(E_(3)),Miocene(N_(1)),Pliocene(N_(2)),and Quaternary(Q),respectively.They can be well correlated with the episodic subsidence and sedimentation occurred in the rifted basins.The distribution of the height and width of the denudational-surfaces is variable along the mountains.The controls on landscape development for the Langshan Mountains-Seertengshan Mountains include: 1)the amount of surface uplift and the time-length of denudation,2)the potential influence of fluvial erosion on local relief,3)the relative intensity of uplift and erosion rates,and 4)the combined effects of tectonic movement,erosion,and isostasy.
%K denudational-surface sequence
%K rifting
%K regional surface uplift
%K denudation
%K landscape development
%K Langshan Mountains- Seertengshan Mountains
%K Inner Mongolia<br>剥蚀面序列
%K 裂谷作用
%K 区域性地面隆起
%K 剥蚀作用
%K 景观发育
%K 内蒙古狼山-色尔腾山
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=EA07051745CDC8D89D5F01A3A4CFE6A9&aid=9982C42C0DBABD43&yid=37904DC365DD7266&vid=96C778EE049EE47D&iid=CA4FD0336C81A37A&sid=A4FA325EA800C820&eid=D767283A3B658885&journal_id=1001-7410&journal_name=第四纪研究&referenced_num=0&reference_num=35