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High-resolution Sequence Stratigraphic Characteristic and Lithological Reservoir Prediction of section, of Qingshuihe Formation in the Central of Junggar Basin

Yang Xu

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Abstract

Based on the principal of base-level cycle, one long-term stratigraphic cycle, two intermediate-term stra-tigraphic cycles and five short-term stratigraphic cycles can be identified in Mem. 1 of Qingshuihe Formation (K1q1) through the drilling data, cores and well-log data. In the MSC1 of intermediate-term stratigraphic cycle, the main deposition is braided-river delta. In the MSC2 of intermediate-term stratigraphic cycle, the main deposition is of lacustrine facies , with some deposition of braided-river delta in the local area. This kind of configuration makes it very comfortable for the development of lithological reservoirs. The regional interlayer develops in the top of unsymmetrical long-term stratigraphic cycle. The favorable reservoir is mainly formed during the early period when the intermediate-term base-level ascended.

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Based on the principal of base-level cycle, one long-term stratigraphic cycle, two intermediate-term stra-tigraphic cycles and five short-term stratigraphic cycles can be identified in Mem. 1 of Qingshuihe Formation (K1q1) through the drilling data, cores and well-log data. In the MSC1 of intermediate-term stratigraphic cycle, the main deposition is braided-river delta. In the MSC2 of intermediate-term stratigraphic cycle, the main deposition is of lacustrine facies , with some deposition of braided-river delta in the local area. This kind of configuration makes it very comfortable for the development of lithological reservoirs. The regional interlayer develops in the top of unsymmetrical long-term stratigraphic cycle. The favorable reservoir is mainly formed during the early period when the intermediate-term base-level ascended.

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Available abstract

Based on the principal of base-level cycle, one long-term stratigraphic cycle, two intermediate-term stra-tigraphic cycles and five short-term stratigraphic cycles can be identified in Mem. 1 of Qingshuihe Formation (K1q1) through the drilling data, cores and well-log data. In the MSC1 of intermediate-term stratigraphic cycle, the main deposition is braided-river delta. In the MSC2 of intermediate-term stratigraphic cycle, the main deposition is of lacustrine facies , with some deposition of braided-river delta in the local area. This kind of configuration makes it very comfortable for the development of lithological reservoirs. The regional interlayer develops in the top of unsymmetrical long-term stratigraphic cycle. The favorable reservoir is mainly formed during the early period when the intermediate-term base-level ascended.

Key concepts: Geology, Facies, Structural basin, Sequence stratigraphy, Delta, Term (time), Deposition (geology), Period (music)

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High-resolution Sequence Stratigraphic Characteristic and Lithological Reservoir Prediction of section, of Qingshuihe Formation in the Central of Junggar Basin — Research Paper | ScholarLens