High-resolution Sequence Stratigraphic Characteristic and Lithological Reservoir Prediction of section, of Qingshuihe Formation in the Central of Junggar Basin
Yang Xu
Abstract
Yang Xu
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.
Key concepts: Geology, Facies, Structural basin, Sequence stratigraphy, Delta, Term (time), Deposition (geology), Period (music)