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《Chinese Journal of Geophysics》 1994-06
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XUE AI-MIN;YANG XIAO-MAO(Institute of Geophysics,Academia Sinica,Beijing 100101)  
Based on six specimen apatite fission track data and geological exploration data in Hefei Basin,authors inversed the geothermal variation of the sedimental rocks and evaluated the subsidence and erosion rates of the basin evolution process.The simulated results are in correspondence with the inferences from other geological data.It could be indicaetd that the tectonic development and thermal histories of the sediments In the south part of the basin differed from the north.The rocks of up Jurassic near to Dabie mountain may bear the paleotemperature up to 120℃ or more during the earlier Cretacous; the tectonic uplift and large erosion(erosion rate≈130 m/Ma) Made the paleotemperature of the rocks decreased to 30-40℃;From late Cretacous,the tectonic environment of south part of the basin was kept going on fluctuation uplift stages.But,In north part of the basin,the highest paleotempelature of late Jurassic and earlier Cretacous rocks was upto 100℃.more,and the lowest was downto 30-60℃ because of the tectonic uplift and erosion (erosion rate≈190 m/Ma, short time)during cretacous.In earlier Tertiary Period,the Paleotemperature of the rocks increased again to about 80℃ because of local rifting(the subsidence rate≈60 m/Ma).Analyzing the thermal histories,subsidence and erosion rates and geologicalexploration data,we conclude that the tectonic evolution in Hefei Basin could be classified into four terms,formation,uplifting,local rifting and re-uplifting.
【CateGory Index】: P313
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