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- W2365248110 abstract "Some lower-crust ductile shear zones(DSZ) occurred in Daqingshan area of Inner Mongolia.,The DSZ lie mainly at the boundaries of different lithology,charactered by well developed,steeply-dipping banding and S—C fabrics.The alternating distribution of high strain zones and low strain zones in the DSZ may be reasonably explained by deformation partitioning.Microstructural study showed that the characters of tectonic gneiss of lower crust DSZ were obviously different from those of mylonites developed in the middle crust.The tectonic gneiss of the lower crust was characterized by well developed banding foliation without porphyroclasts or matrix,which may be resulted from partial melting of rock.Meanwhile,feldspar grains in the gneiss touch each other with triple point configuration,suggesting that the rock deformation mechanism in lower crust was controlled mainly by diffusion creep and granular flow strengthened by melt.Garnet-biotite geothermobarometry analysis revealed a high amphibolite-granulite metamorphic facies with a deformation temperature of 710 ℃ and a confining pressure of 0.6 GPa.The 1 900 Ma～2 200 Ma age obtained by single zircon isotopic dating from the intrusive body in the gneiss demonstrated that the DSZ was formed in the early Proterozoic period.It was considered that the DSZ was resulted from the horizontal convergence of Yinshan land mass and Eerduosi land mass in a NNE-SSW direction." @default.
- W2365248110 created "2016-06-24" @default.
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- W2365248110 date "2008-01-01" @default.
- W2365248110 modified "2023-09-26" @default.
- W2365248110 title "THE CHARACTERS AND GENESIS OF THE LOWERCRUST DAQINGSHAN DUCTILE SHEAR ZONES IN THE INNER MONGOLIA" @default.
- W2365248110 hasPublicationYear "2008" @default.
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