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《ACTA SEDIMENTOLOGICA SINICA》 1998-01
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Application of Vitrinite Reflectance in Reconstruction of Paleotemperature: Evolution of Paleotemperature in the Eastern and Western Mesozoic-Cenozoic Sedimentary Basins,China

Zou Huayao; Wu Zhiyong(Jianghan Petroleum Institute,Hubei Jinzhou 434102)  
Comparison and discussion were carried out with various methods,using vitrinite reflectance(VR) to reconstruct paleotemperature of sedimentary basins. It was perceived that the Easy R0 algorithm is the most accurate method for prediction of VR and then for palcotemperature throughout the range Of organic maturity normally encountered. The Easy R0 model was wsed to restore paleotemperature gradients(PG) of four sedimentary basins in the eastern and western China,respectively. It was indicated that the eastern basins characteristic of continental rift basin had higher paleotemperature gradients in the Mesozoic-Cenozoic Era than those characteristic of foreland basin in the western China. The eastern basins had more than 4. 0℃/100m of PG from the Late Mesozoic to Early Cenozoic Era,but lower than 3. 0~2. 5℃/100m in the western basins of China during the same period. Three of the four basins concerned, Liaohe Basin,subei Basin in the east and santanghu Basin in the west,had a decreasing evolution in PG in Late Mesozoic,while Qaidarn Basin underwent an increasing evolution in PG,from 2. 5℃ /100m to nowadays 3. 0℃ /100m. The success of PG reconstructions for four basins suggested that the Easy R0 algorithm is suitable to PG reconstruction of various tectonically different basins.
【CateGory Index】: P544.4
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