Analyses of the Rock Magnetic Fabric, Deformation and Kinematics in the Qifengcha Liulimiao Area, Huairou County,Beijing
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

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.