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- W2354244510 abstract "The Cretaceous strata of the Hefei Basin are divided into two series and four formations with distinctive lithological features,which are mainly sourced from the Dabie and Zhangbaling organic belts.Extensional deformation by large-scaled right-lateral strike slip at the initial period of Cretaceous led to release of underground thermal energy forming the basin.Differential uplift of the basin was resulted from basin-range episodic tectonism and deep-fault strike slip at the early Cretaceous.The basin entered the stage of initial depression due to stress relief and overall uneven uplift at the late Cretaceous.Finally,the stress relief turned to SW-NE trending compression giving birth to the dustpan-like rift basin." @default.
- W2354244510 created "2016-06-24" @default.
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- W2354244510 date "2007-01-01" @default.
- W2354244510 modified "2023-09-23" @default.
- W2354244510 title "CRETACEOUS STRATA OF THE HEFEI BASIN AND THE BASINAL EVOLUTION" @default.
- W2354244510 hasPublicationYear "2007" @default.
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