Sequence Stratigraphic Analysis of Badaowan Formation in Dishuiquan Area, Junggar Basin

Zhe Wang; Zhen Kui Jin; Gui Zai Li

doi:10.4028/www.scientific.net/AMR.616-618.56

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HomeAdvanced Materials ResearchAdvanced Materials Research Vols. 616-618Sequence Stratigraphic Analysis of Badaowan...

Sequence Stratigraphic Analysis of Badaowan Formation in Dishuiquan Area, Junggar Basin

Abstract:

In the light of the principle and method of sequence stratigraphy, the sequence stratigraphic framework of Badaowan formation in the Dishuiquan area was established. The results show that the sequence of Badaowan formation is one and half, including 5 system tracts. The whole experiences the process of retrogradation, progradation and then retrogradation again. There develop three types of sedimentary facies such as braided river, braided river delta and lakes, five types of sedimentary subfacies and 10 types of sedimentary microfacies. Most of JSQ1 sequence lowstand system tract is braided rivers, the lacustrine transgressive system tract mainly develops shore-shallow lacustrine sediment and most of highstand system tract is braided river delta; lowstand systems tract of JSQ2 sequence mainly develops braided river delta, most of the lacustrine transgressive system tract is shore-shallow lacustrine sediments.

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Periodical:

Advanced Materials Research (Volumes 616-618)

Pages:

56-59

DOI:

https://doi.org/10.4028/www.scientific.net/AMR.616-618.56

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Online since:

December 2012

Authors:

Zhe Wang, Zhen Kui Jin, Gui Zai Li

Keywords:

Badaowan Formation, Dishuiquan Area, Junggar Basin, Lake Basin Deposition, Sequence Stratigraphy, System Tract

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References

[1] Xuanjun Yuan, Liangqing Xue, Yingliu Chi, et al: Acta Petrolei Sinica, Vol. 24(3)(2003), pp.11-15(in Chinese)..

Google Scholar

[2] Wei Dong, Changsong Lin, Chenggang Qin, et al: Geoscience, Vol. 22(5)(2008), pp.794-802(in Chinese).

Google Scholar

[3] Ping HU, Heng XU, Xinbing LI, et al. Acta Sedimentogica Sinica, Vol. 24 (3)(2006), pp.377-386(in Chinese)..

Google Scholar

[4] Xiaomin ZHU, An KANG, Qin ZHANG, et al. Oil& Gas Geology, Vol. 23(2)(2002), pp.121-126(in Chinese)..

Google Scholar

[5] Renchong WANG, Huaimin XU, Loujun LIU, et al. Petroleum Exploration and Development, Vol. 36(5)(2009), pp.601-608(in Chinese)..

Google Scholar

[6] Van Wagoner, J.C., Posamentier, H.W., Mitchum, R.M., et al. SEPM Special Publication, 1988, pp.39-45.

Google Scholar

[7] Van Wagoner J C, Mitchum R M, Campion K M, et al. Houston: AAPG Methods in Exploration, 1990, pp.1-55.

Google Scholar