%0 Journal Article
%T Paleocurrent direction of the Late Cenozoic sedimentary sequence of the Tibetan plateau northwestern margin constrained by AMS and its tectonic implications<br>青藏高原西北缘晚新生代沉积岩古流向的磁化率各向异性确定及其构造意义
%A PEI JunLing
%A SUN ZhiMing
%A LI HaiBing
%A SI JiaLiang
%A PAN JiaWei
%A LIU Jing
%A LIU XueGang
%A ZHAO Yue
%A <br>裴军令
%A 孙知明
%A 李海兵
%A 司家亮
%A 潘家伟
%A 刘静
%A 刘雪刚
%A 赵越
%J 岩石学报
%D 2008
%I 
%X The determination of paleocurrent directions is a robust approach to establish the sediments transport and of the deposition progress.The credibility of the Anisotropy of Magnetic Susceptibility(AMS)as a paleocurrent indicator has been known from work on naturally and laboratory deposited sediments.The study of 80 samples magnetic fabric has been developed for the Late Cenozoic strata including Wuqia,A'tushi and Xiyu Formations,Kekeya section of the Tibetan plateau northwestern margin.Flinn-type( F versus L...
%K Paleocurrent directions
%K Anisotropy of Magnetic Susceptibility
%K Late Cenozoic
%K West Kunlun Mountain
%K Uplift<br>古流向
%K 磁化率各向异性
%K 晚新生代
%K 西昆仑
%K 隆升
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=C52FFDB1CFBC14719EF6952E8EB1B178&yid=67289AFF6305E306&vid=B91E8C6D6FE990DB&iid=DF92D298D3FF1E6E&journal_id=1000-0569&journal_name=岩石学报&referenced_num=6&reference_num=26