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Zhou Shitao, Wan Guangguan, Liu Yongkang. The Criteria on Maturity of Organic Materials in Carbonate Rocks by Ion Microprobe[J]. Acta Sedimentologica Sinica, 1997, 15(2): 31-34.
Citation: Zhou Shitao, Wan Guangguan, Liu Yongkang. The Criteria on Maturity of Organic Materials in Carbonate Rocks by Ion Microprobe[J]. Acta Sedimentologica Sinica, 1997, 15(2): 31-34.

The Criteria on Maturity of Organic Materials in Carbonate Rocks by Ion Microprobe

  • Received Date: 1996-06-12
  • Publish Date: 1997-04-10
  • he secondary ions of the hydrocarbon fragments suchas CH, CH3 and benzene series homologues,etc. can be detected by ion microprobe(SIM S) in the organic analysis of carbonate rocks. There is a close relationship of the peak and its abundance of these fragment ions with the themical com posi do nand molecular structure of the organic materials detected. There is certain regularity with the change ofCH/C and CH3 /C ratios which could reach the maximum at theoil forming period. And the value of themethyl ratio between arene compounds and benzene serial homologues can reflect the cha ng a of o rganicmatuity and shown good linear relationship vitrinite reflectance(R).This paper represented part of theexperimental results obtained during the study of the oil and soure rock correlation and oil-gas evolutionof marine carbonate rocks in the Yunnan, Guizhou and Guangxi area by using SIM S.
  • [1] 1 Alan Bmwn and加hn C V ikerman. Static S1M S FABM S andS1MS hnaging in Applied Surface Analysis. The Analyst,1984, 109(7): 851-859.

    2 李树枝.金奎励.无定形体的离子探针研究.石油与天然气地质.1990, 11(4): 463-466.

    3 周士涛.离子探针质谱及其在地学中的应用.地质与地球化学.1987.(3): 69-73.

    3 J M享特.石油地球化学和地质学.北京:石工业出版社. 1986.
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  • Received:  1996-06-12
  • Published:  1997-04-10

The Criteria on Maturity of Organic Materials in Carbonate Rocks by Ion Microprobe

Abstract: he secondary ions of the hydrocarbon fragments suchas CH, CH3 and benzene series homologues,etc. can be detected by ion microprobe(SIM S) in the organic analysis of carbonate rocks. There is a close relationship of the peak and its abundance of these fragment ions with the themical com posi do nand molecular structure of the organic materials detected. There is certain regularity with the change ofCH/C and CH3 /C ratios which could reach the maximum at theoil forming period. And the value of themethyl ratio between arene compounds and benzene serial homologues can reflect the cha ng a of o rganicmatuity and shown good linear relationship vitrinite reflectance(R).This paper represented part of theexperimental results obtained during the study of the oil and soure rock correlation and oil-gas evolutionof marine carbonate rocks in the Yunnan, Guizhou and Guangxi area by using SIM S.

Zhou Shitao, Wan Guangguan, Liu Yongkang. The Criteria on Maturity of Organic Materials in Carbonate Rocks by Ion Microprobe[J]. Acta Sedimentologica Sinica, 1997, 15(2): 31-34.
Citation: Zhou Shitao, Wan Guangguan, Liu Yongkang. The Criteria on Maturity of Organic Materials in Carbonate Rocks by Ion Microprobe[J]. Acta Sedimentologica Sinica, 1997, 15(2): 31-34.
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