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APPLICATION OF CARBON AND OXYGEN ISOTOPES TO CARBONATE SEQUENCE STRATIGRAPHY:ANALYSIS OF MAPING FORMATION,SOUTHERN GUIZHOU PROVINCE

Li Rufeng (University of Petroleum,Beijing 102200) Liu Benpei (Department of Geology and Mineral Resources,China University of Geosciences,Beijing 100083)  
Combined with the analysis of caronate sequence stratigraphy,the stable isotope (δ 13 C,δ 18 O)values of Maping Formation (Gzelian-Asselian)are systematically measured. Then,the relations of their evolution to the sequence stratigraphy are discussed. The research results indicate that the δ 13 C values of parasequence decreases upward,while the δ 13 C values of transgressive systems tract(TST) and high stand systems tracts (HST) generally trend to increase and decrease respectively. The δ 13 C and δ 18 O values show obviously the negative anomaly at the sequence boundaries. It is also pointed out that the δ 13 C occurrence and evolution of the sequence stratigraphy are mainly controlled by the periodic variation of golbal glacio eustasy.
【Fund】: 国家科委基础研究重大项目
【CateGory Index】: P53
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