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Geoscience ›› 2006, Vol. 20 ›› Issue (1): 77-85.

• Engineering Geology and Environmental Geology • Previous Articles     Next Articles

The Characteristics of the Braided-river Delta of the Lower Jurassic Sangonghe Formation of the Haojiagou Section in the Southern Part of the Junggar Basin

LIU Zhi-rong1,WANG Xun-lian1,ZHOU Hong-rui1,DENG Hong-wen2,HONG Shun-ying3   

  1. 1 School of Earth and Resources, China University of Geosciences, Beijing100083, China;
    2 School of Energy Resources, China University of Geosciences, Beijing100083, China;
    3 Institute of Earthquake Science, China Earthquake Administration, Beijing100036, China
  • Received:2005-07-14 Revised:2005-10-14 Online:2006-01-20 Published:2006-01-20

Abstract:

The sedimentary facies and high-resolution sequence stratigraphy of the Lower Jurassic Sangonghe Formation in the southern part of the Junggar Basin are discussed. It is believed that there are typical deposits of braided-river delta in the Sangonghe Formation. The braided-river delta can be divided into three subfacies. They are braided-river deltaic plain subfacies, braided-river deltaic front subfacies and pro-braided-river delta subfacies. Almost all deposits of the braided-river delta are finer clastic rocks including sandstone, silty sandstone and mudstone, except that a few beds of coarse deposits occur in braided-river channel microfacies. The Sangonghe Formation can be divided into 2 middle-term base-level cycles: MSC1 and MSC2. The MSC1 can be subdivided into 4 short-term base-level cycles: SSC1, SSC2, SSC3 and SSC4; and the MSC2 develops incompletely.

Key words:  braided-river delta, high-resolution sequence stratigraphy, Lower Jurassic, the Junggar Basin, the Sangonghe Formation, base-level cycle

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