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《Chinese Journal of Geology(Scientia Geologica Sinica)》 2007-04
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GEOCHEMICAL CHARACTERISTICS OF PALEOGENE MUDSTONES IN THE BOXING SAG NORTH OF THE WEST SHANDONG RISE AND THEIR TECTONIC IMPLICATIONS

Han Denglin1 Li Zhong1 Li Shuangying2 Xu Chengwu1 Long Lingli1(1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029;2.College of Resources and Environmental Engineering,Hefei University of Technology,Hefei 230009)  
The application of detrital geochemistry to determine provenance attribute is an important method for basin analysis.Geochemical characteristics of 20 mudstone samples from the Eocene and Oligocene deposits in the Boxing Sag,Jiyang Depression of Bohai Bay Basin,showed that the REE distribution pattern was similar to that of the upper continental crust.They were characterized by enrichment of LREE,flat HREE pattern and slightly negative Eu anomaly.Although the ratios of trace elements showed the materials of the source rocks for both the Eocene and the Oligocene deposits being drived from the post-Archean strata,there was an obviously difference between the materials of the source rocks between the Eocene and Oligocene deposits.According to the discrimination diagram for attribute of source rocks,the source rocks of Eocene deposits were mainly felsic volcanics,while that of Oligocene deposits were felsic and basic volcanics.The great difference between the source rocks of Eocene and Oligocene deposits suggested that there existed a clear change in provenance supply between Eocene and Oligocene,which might be resulted from the uplifting of western Shandong area,namely,a tectonic differentiation between the West Shandong Rise and neighbouring basins,which influenced oil-gas accumulation and reservoir in the Paleogene basins.
【Fund】: 国家自然科学基金项目(批准号:40672083)资助
【CateGory Index】: P594
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