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《Geology of Anhui》 2007-04
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CRETACEOUS STRATA OF THE HEFEI BASIN AND THE BASINAL EVOLUTION

DU Chang-zhou,SUN Ya-li,ZHANG Li-ming(No.312 Geological Team of Anhui Bureau of Geology and Mineral Resources Exploration,Bengbu 233040,China)  
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.
【CateGory Index】: P534.53
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