%0 Journal Article
%T Analyses of the Rock Magnetic Fabric, Deformation and Kinematics in the Qifengcha Liulimiao Area, Huairou County,Beijing<br>北京怀柔崎峰茶-琉璃庙地区岩石磁组构特征及其构造意义
%A CHEN Bai-lin
%A LI Zhong-jian
%A XIE Yan-xia
%A <br>陈柏林
%A 李中坚
%A 谢艳霞
%J 地球学报
%D 1997
%I 
%X The magnetic fabric means the anisotropy of the susceptibility. The characteristics of the rock magnetic fabric in Qifengcha Liulimiao area are that the value of P which symbolizes the degree of the magnetic anisotropy is high, the value of E symbolizing the ellipsoidel flattening is above zero, the magnetic schistosity is well developed and the magnetic lineation is poor. The analytical results of the magnetic fabric show that the regional structural deformation is strong, of which the flaser deformation is the chief, the west side of the NS trending structural zone moved down with respect to the east side and the hanging wall of the WE trending structural zone thrusted up with respect to the foot wall from south to north.
%K the Qifengcha Liulimiao area
%K magnetic fabric
%K structural deformation<br>北京
%K 崎峰茶－琉璃庙
%K 磁组构
%K 构造变形分析
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=1DF69A47DE80569EC8F859DF61571180&aid=8A5BBB6F6CE57A26F0FEB5FEB95CC373&yid=5370399DC954B911&vid=13553B2D12F347E8&iid=0B39A22176CE99FB&sid=03A030BB0C519C60&eid=A8DE7703CC9E390F&journal_id=1006-3021&journal_name=地球学报&referenced_num=19&reference_num=0