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- W2353607666 abstract "There is obvious geological difference existing between west part and east part of north Qinling structure zone in Henan province,mainly showing the characteristics of structures of different grades highly developed eastwardly while metamorphism also strengthened and mineral assemblages became more complicated in same orientation.The main reasons for all those phenomena are gradual collision,impact of obduction nappe structure movement and stratum rising and falling caused by late developed fractures." @default.
- W2353607666 created "2016-06-24" @default.
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- W2353607666 date "2010-01-01" @default.
- W2353607666 modified "2023-09-26" @default.
- W2353607666 title "The deference between west and east part of north Qinling structure zone in Henan province and its genesis" @default.
- W2353607666 hasPublicationYear "2010" @default.
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