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- W2367887249 abstract "Based on the study of the mottled structure of the Shuangqiaoshan Group metamorphic rock in Dabeiwu area, Jiangxi province, the authors discover the syngenetic clast for the fisrt time in the area. As a structural phenomenon representing a turbulent sedimentary environment, syngenetic clast in sedimentary rock provides a strong support to the view that the Shuangqiaoshan Group is a turbidite. There mainly occur two type deformations in the area. One is an appressed fold and the other is a ductile shear zone. By equilibrium diagram, it is calculated that the shorting ratio caused by appressed fold in the area is about 71.6%. The Dabeiwu ductile shear zone, formed in the epimetamorphic clastic rocks, has typical features and particular discerning signs. According to the strain measurements of syngenetic clast and syntectonic porphyroclast, the shear strain(γ) of Dabeiwu ductile shear zone is about 1.01～2.13 and the shear displacement is about 0.6～0.8km, while the intrastratal compressed ratio of Shuangqiaoshan Group is about 23.1～45.3%. Combining to the analysis of the evolution history of regional structure, the authors believe that the Shuangqiaoshan Group in the area has undergone two phases of deformation. The former is the appressed fold formed in Jinning epoch with the forming and deforming of the basement rock system of Yangzi platform. The latter is the ductile shear deformation occurred in the Yanshan epoch and related to the emplacement and upwelling of Ehu granitic intrusive, which caused the vertical ductile shear deformation in the metamorphic rock of the northwest side." @default.
- W2367887249 created "2016-06-24" @default.
- W2367887249 creator A5035061771 @default.
- W2367887249 date "2002-01-01" @default.
- W2367887249 modified "2023-09-25" @default.
- W2367887249 title "Analysis of the depositional environment and deformation history of Shuangqiaoshan Group——An example from Dabeiwu area, Jiangxi provinc" @default.
- W2367887249 hasPublicationYear "2002" @default.
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