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- W2355993567 abstract "Field work shows that there were mainly two-stage deformations in Kangxian segment of Mianlue tectonic zone.The early was mainly characterized by ductile deformation in deep level,and the late,brittle-ductile deformation in shallow-level,such as brittle faults,which cut the tight folds and penetrability foliations formed in the early stage.However,the magnetic fabric mainly revel the latest deformation features.The magnetic samples totally yield a higher PJ(magnetic susceptibility anisotropy),which reflect an intense deformation in its history.The T and E reflect the strains of compression and shearing,which are consistent with the result of Filinn Diagram.The magneticfoliations concentrated in two groups with the average occurrences of 344°∠40° and 179°∠61° exposed conjugate in plane,and the acute angle bisectors distribute nearly E-W,which may hint that the N-S compression with E-W strike-slip in the tectonic zone.The magnetic lineation totally shares a low dip-angle,nearly E-W.High angle magnetic foliations and the domain low angel magnetic lineation reflect the compression with strike-slip deformation,and partial high magnetic lineation related to thrusting.The minimum susceptibility show nearly N-S stress in the late stage.Combating the magnetic fabric results and structural analysis,we conclude that the late compressed and dextral strike-slip revealed that west Qinling developed dextral strike-slip caused by the block-off of Bikou Terrain during the southward thrust,and also proved that Bikou Terrain escaped to west." @default.
- W2355993567 created "2016-06-24" @default.
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- W2355993567 date "2013-01-01" @default.
- W2355993567 modified "2023-09-23" @default.
- W2355993567 title "Characteristics of magnetic fabric and its significance in Kangxian segment of Mianlüe tectonic zone" @default.
- W2355993567 hasPublicationYear "2013" @default.
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