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- W2376980711 abstract "The Jiamusi-Yitong falut was the western branch of northern extension of Tan-Lu fault,which controlled the distributions of many basins within Jia-Yi graben. The authous found a ductile-brittle shear zone with trend of NNE in Shuiquliu of Shulan area. Combining the microstructure study,the authors consider that the shear zone was consisted of protomylonite-mylonite and displayed sinistral strike-slip shear characteristics. With the measurement of finite-strain determination( Fry measurement),the strain type of the study area was considered to be extension strain. EBSD( electron back scatter diffraction) measurement also indicated the study area had undergone a sinistral strike-slip shear zone and quartz fabrics were mainly low-middle temperature prism-glide fabrics with slip system of { 0001} 110 . To sum up,Shuiquliu shear zone had experienced a sinistral strike-slip shearing in middle-late Early Cretaceous,which was related to moving direction changing from NWW to NNW of the western Pacific Izanagi plate obliquely subducting under the Eurasia plate." @default.
- W2376980711 created "2016-06-24" @default.
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- W2376980711 date "2013-01-01" @default.
- W2376980711 modified "2023-09-27" @default.
- W2376980711 title "Characteristics of ductile deformation of Jiamusi-Yitong fault" @default.
- W2376980711 hasPublicationYear "2013" @default.
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