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《Journal of Jilin University(Earth Science Edition)》 2006-02
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Basin Tectonic Setting and Paleoclimate Revealed from Minerals and Geochemistry of the Sediments

WANG Guo-dong,CHENG Ri-hui,YU Min-feng,JIANG Xue,CUI Kun-ningCollege of Earth Sciences,Jilin University,Changchun130061,China  
Changes of tectonic setting and climate are two important controlling factors for basin filling and evolution.They control the types and the distributions of the sediments.In the view of mineralogy and geochemistry of sediments,some dominating parameters are used to study the evolution of the basin tectonic setting and climate in the geological history,including δ~(13)C and δ~(18)O of carbonates,quartz/feldspar,kaolinite/clay and illite/clay.The low value of the quarter/feldspar occurred in Quan Ⅲ and Quan Ⅳ sequences indicates that there were tectonic activities happened at that time.The analyses of illite/clay and kaolinite/clay show that the climate had undergone the changes from aridity in the Quan Ⅲ period to humidity in the Qingshankou period,quickly to aridity in the Yaojia period,to humidity in the NenⅠperiod, and to hot humidity in the Nen Ⅲ and Ⅳ period during the Middle Cretaceous in Songliao Basin.The analysis of the stable isotope of carbon and oxygen from the carbonates shows that there was a transgression event at 83.3 Ma and a regression event at 82.8 Ma in SongliaoBasin.
【Fund】: 国家“973”项目(2006CB701403)
【CateGory Index】: P544.4
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