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- W2362974227 abstract "Eastern Jiaodong,regionally located at the eastern end of the Qinling-Dabie-Sulu orogenic belt,is a Mesozoic strike-slip thrust belt.The study of ultramicroscopic structure is favorable to solving the problem of deformation mechanisms of rocks.Microstructure and ultramicrostructure of the strike-slip thrust belt in eastern Jiaodong have been studied using both microscopy and TEM.Study indicates that the dislocation substructure of quartz in the main strike-slip thrust shear zone is dominated by linear dislocation,and in addition,dislocation loops,bow-out,walls,arrays and net and subgrains are also common.A middle-to low-temperature,plastic deformation environment.can be deduced from the ultramicroscopic dislocation structures of quartz.Furthermore,the average differential paleo-stress values of the Shidao,Rongcheng and Mouping shear zones show a trend of gradual decrease,which seems to be inversely correlated with the trend of temperatures." @default.
- W2362974227 created "2016-06-24" @default.
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- W2362974227 date "2005-01-01" @default.
- W2362974227 modified "2023-09-24" @default.
- W2362974227 title "Ultramicrostructure of the Mesozoic strike-slip thrust belt in eastern Jiaodong" @default.
- W2362974227 hasPublicationYear "2005" @default.
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