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Volume 28 Issue 6
Nov 2017
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Ruohan Liu, Zaixing Jiang, Ming Wang, Weili Yang, Jingxiang Guo, Minghao Wu, Yi Gao, Shanyazi Wei, Zhihong Nie, Hong He. Reservoir Characteristics and Controlling Factors of Silurian Lower Kepingtage Formation in Tahe Area, Tarim Basin, NW China. Journal of Earth Science, 2017, 28(6): 1135-1144. doi: 10.1007/s12583-016-0941-8
Citation: Ruohan Liu, Zaixing Jiang, Ming Wang, Weili Yang, Jingxiang Guo, Minghao Wu, Yi Gao, Shanyazi Wei, Zhihong Nie, Hong He. Reservoir Characteristics and Controlling Factors of Silurian Lower Kepingtage Formation in Tahe Area, Tarim Basin, NW China. Journal of Earth Science, 2017, 28(6): 1135-1144. doi: 10.1007/s12583-016-0941-8

Reservoir Characteristics and Controlling Factors of Silurian Lower Kepingtage Formation in Tahe Area, Tarim Basin, NW China

doi: 10.1007/s12583-016-0941-8
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  • Corresponding author: Zaixing Jiang, jiangzx@cugb.edu.cn
  • Received Date: 09 Oct 2016
  • Accepted Date: 12 Feb 2017
  • Publish Date: 01 Dec 2017
  • With the breakthrough of exploration in Well TP16-1, the lower Kepingtage Formation becomes a key target for petroleum exploration of deep clastic reservoir in Tahe area. In this paper we focused on the research of the reservoir characteristics and its controlling factors in two sub-member formations (S1k11 and S1k13). Based on X-ray diffraction, conventional physical properties data (porosity and permeability) and reservoir storage space data (casting thin section and scanning electron microscope), we determined that the S1k1 Formation belongs to extra-low porosity and permeability reservoir, although the upper S1k13 Formation shows relative better physical characteristic than the lower S1k11 Formation. The development of storage space in the study area is controlled by sedimentary microfacies, diagenesis process. Reservoirs in S1k1 Formation are mainly located in channel (S1k11 sandstones) and sand flat (S1k13 sandstones). The sand flat sediments with a more coarse grain size compared with the channel. In diagenesis, compaction is the major controlling factor for reducing the porosity, followed by cementation. Dissolution of diagenesis is the major controlling factor in enhancing the reservoir porosities. Compared with channel (S1k11) sandstones, sand flat sandstones (S1k13) have better reservoir quality for its weaker compaction, cementation and stronger dissolution. On the basis of sedimentary characteristics (grain size and subfacies), physical property (porosity and permeability) and reservoir storage space, we divide the S1k1 reservoir into three categories (Ⅰ, Ⅱ and Ⅲ). Type Ⅰ reservoir is high quality reservoir. It is mainly distributed in the south area of S1k11 and S1k13 reservoir. Type Ⅱ is moderate reservoir. It is located in the middle of S1k11 reservoir and in the north of S1k13 reservoir. Type Ⅲ is the poor reservoir. It is only located in the north of S1k11 reservoir.

     

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