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ZHANG Shiguang. Application of HighResolution Sequence Stratigraphy in the Study of the Reservoir Macroheterogeneity:Taking the Fuyu oil layer of Chao 1Chaoqi 3 blocks in Chaoyanggou oil reservoir of Songliao Basin as an example[J]. Acta Sedimentologica Sinica, 2009, 27(3): 458-469.
Citation: ZHANG Shiguang. Application of HighResolution Sequence Stratigraphy in the Study of the Reservoir Macroheterogeneity:Taking the Fuyu oil layer of Chao 1Chaoqi 3 blocks in Chaoyanggou oil reservoir of Songliao Basin as an example[J]. Acta Sedimentologica Sinica, 2009, 27(3): 458-469.

Application of HighResolution Sequence Stratigraphy in the Study of the Reservoir Macroheterogeneity:Taking the Fuyu oil layer of Chao 1Chaoqi 3 blocks in Chaoyanggou oil reservoir of Songliao Basin as an example

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  • Corresponding author: ZHANG Shiguang
  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2009-06-10
  • In application to highresolution sequence stratigraphy principles and methods, forty one shortterm baselevel cycles and seven middleterm baselevel cycles and two longterm baselevel semicycles in Fuyu oil layer of Chao 1 Chao gas 3 blocks of Chaoyanggou oil field are identified. By the sedimentary dynamics analysis of genesis of multiage baselevel cycles, quantitative analysis of the core testing and statistical data which characterize the macroscopic heterogeneity of the reservoir, we point out that with the uprising of the longterm baselevel cycle, inlayer heterogeneity of shortterm baselevel cycles becomes stronger, and interlayer heterogeneity of middleterm baselevel cycles becomes weaker, and plane heterogeneity of shortterm baselevel cycles becomes stronger. With the subsiding of the longterm baselevel cycle, every trend is contrary. By analysis, the changes of sedimentary environment that are caused by the changes of baselevel cycles and associated accommodation are the determinative factors for feature differences of reservoir macroscopic heterogeneity.
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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  • Received:  1900-01-01
  • Revised:  1900-01-01
  • Published:  2009-06-10

Application of HighResolution Sequence Stratigraphy in the Study of the Reservoir Macroheterogeneity:Taking the Fuyu oil layer of Chao 1Chaoqi 3 blocks in Chaoyanggou oil reservoir of Songliao Basin as an example

    Corresponding author: ZHANG Shiguang

Abstract: In application to highresolution sequence stratigraphy principles and methods, forty one shortterm baselevel cycles and seven middleterm baselevel cycles and two longterm baselevel semicycles in Fuyu oil layer of Chao 1 Chao gas 3 blocks of Chaoyanggou oil field are identified. By the sedimentary dynamics analysis of genesis of multiage baselevel cycles, quantitative analysis of the core testing and statistical data which characterize the macroscopic heterogeneity of the reservoir, we point out that with the uprising of the longterm baselevel cycle, inlayer heterogeneity of shortterm baselevel cycles becomes stronger, and interlayer heterogeneity of middleterm baselevel cycles becomes weaker, and plane heterogeneity of shortterm baselevel cycles becomes stronger. With the subsiding of the longterm baselevel cycle, every trend is contrary. By analysis, the changes of sedimentary environment that are caused by the changes of baselevel cycles and associated accommodation are the determinative factors for feature differences of reservoir macroscopic heterogeneity.

ZHANG Shiguang. Application of HighResolution Sequence Stratigraphy in the Study of the Reservoir Macroheterogeneity:Taking the Fuyu oil layer of Chao 1Chaoqi 3 blocks in Chaoyanggou oil reservoir of Songliao Basin as an example[J]. Acta Sedimentologica Sinica, 2009, 27(3): 458-469.
Citation: ZHANG Shiguang. Application of HighResolution Sequence Stratigraphy in the Study of the Reservoir Macroheterogeneity:Taking the Fuyu oil layer of Chao 1Chaoqi 3 blocks in Chaoyanggou oil reservoir of Songliao Basin as an example[J]. Acta Sedimentologica Sinica, 2009, 27(3): 458-469.

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