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- W2390806035 abstract "The Tongbai Mt was thought to be mainly composed of a Tongbai core complex unit,an early Cretaceous granitic gneiss complex that contains some Triassic medium to high grade metamorphic rocks,which,along with the host,had been subjected to late tectonic deformation,forming two big ductile shear zones of completely opposite shearing rotation,one on the southern side and the other on the northern.The Yindian-Malong shear zone in the south is a dextral strike-slip fault by the South China plate that cut the Dabie orogen obliquely as a result of a SSE-NNW compression.Field observations showed a regular pattern for the distribution of metamorphic fluid in the area.This paper,based on researches into geologic features and strike-slip nature of the Yindian-Malong shear zone,metamorphism and deformation of mylonite and mylonitized rock,material composition,deformational feature and material source of felsic veins in the zone,discussed the distribution pattern of metamorphic fluid within the shear zone,and the relationship of metamorphism and deformation with the metamorphic fluid." @default.
- W2390806035 created "2016-06-24" @default.
- W2390806035 creator A5081665965 @default.
- W2390806035 date "2013-01-01" @default.
- W2390806035 modified "2023-09-23" @default.
- W2390806035 title "Metamorphic and deformational features of the metamorphic fluid at the southern fringe of the Tongbai-Dabie Mt" @default.
- W2390806035 hasPublicationYear "2013" @default.
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