%0 Journal Article
%T A Study on Tectonic Stress's Field of Brittle Deformation in the Northern Tibet Qinghai Plateau<br>青藏高原北缘断裂擦痕的构造分析
%A LI You-she
%A CUI Jun-wen
%A GAO Jing
%A TANG Zhe-ming
%A <br>李有社
%A 崔军文
%A 高静
%A 唐哲明
%J 地球学报
%D 1997
%I 
%X Through field observation and computer processing of fault slip data, we divided the brittle tectonic stress' fields in the northern Tibet Qinghai plateau into two periods: Oligocene middle Pleistocene and middle Pleistocene Holocene. The maximum principal stress's orientation is approximately S N direction in the former period and N E in Altyn Taph and N W in Qilian respectively in the latter one. Meanwhile, geodyncmics of the northern Tibet Qinghai plateau is analysized.
%K northern Tibet Qinghai plateau
%K tectonic stress field
%K fault slip
%K computer processing<br>青藏高原北缘
%K 构造应力场
%K 擦痕
%K 计算机处理
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=1DF69A47DE80569EC8F859DF61571180&aid=8A5BBB6F6CE57A26B3E754D33C635E35&yid=5370399DC954B911&vid=13553B2D12F347E8&iid=0B39A22176CE99FB&sid=28F8B56DB6BEE30E&eid=76B5E24D6EC46B4B&journal_id=1006-3021&journal_name=地球学报&referenced_num=1&reference_num=0