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Identification of Diagenetic Facies Based on Diagenetic Process: An Example from Paleogene Lake Sediment Sandstone in Bozhong X Oilfield

Received: 3 June 2018     Accepted: 19 June 2018     Published: 7 July 2018
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Abstract

Based on diagenetic evolution, reservoir diagenetic facies evolution was restored in burial history through quantitatively calculating the original porosity reconstructed by compaction, cementation and dissolution using core measurement data. The essence of this method was illustrated and its effectiveness was demonstrated using Paleogene lake sediment sandstone in Bozhong X oilfield, Bohai Bay Basin, China. Because diagenetic field changes as the structure depth increases or decreases and acts on deposition, diagenetic facies can be significantly different in different geological period. The Ed1 reservoir has experienced such an evolutionary process of W-Com_W-Cla-C_M-Car-C to M-Com_M-Clay-C_W-Qua-C_W-Fel-D_W-Car-D to M-Com_M-Cla-C_W-Qua-C_W-Fel-D_W-Car-D, while the Ed2 , the Ed3 and the Es1 are W-Com_W-Cla-C to M-Com_M-Cla-C-S-Com_S-Clay-C_W-Qua-C_W-Fel-D to S-Com_S-Cla-C_W-Qua-C_M-Fel-D, M-Com_W-Cla-C_W-Qua-C_W-Fel-D to M-Com_M-Cla-C_W-Qua-C_W-Fel-D to S-Com_M-Clay-C_W-Qua-C_S-Fel-D to S-Com_S-Clay-C_M-Qua-C_S-Fel-D and M-Com_W-Cla-C_W-Car-C to M-Com_M-Cla-C_W-Car-C_M-Fel-D_W-Car-D to M-Com_M-Clay-C_S-Fel-D_M-Car-D to S-Com_M-Cla-C _S-Fel-D_ M-Car-D respectively. Through this study, the reason for the dynamic change of sand body in the diagenetic field and the anisotropy of the reservoir are revealed.

Published in Earth Sciences (Volume 7, Issue 4)
DOI 10.11648/j.earth.20180704.13
Page(s) 158-165
Creative Commons

This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.

Copyright

Copyright © The Author(s), 2018. Published by Science Publishing Group

Keywords

Diagenetic Stages, Clastic Sandstones, Bozhong Oilfield, Diagenetic Simulation, Diagenetic Facies

References
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    Qian Wendao, Yin Taiju, Sun Shaochuan, Zhang Changmin, Hou Guowei, et al. (2018). Identification of Diagenetic Facies Based on Diagenetic Process: An Example from Paleogene Lake Sediment Sandstone in Bozhong X Oilfield. Earth Sciences, 7(4), 158-165. https://doi.org/10.11648/j.earth.20180704.13

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    ACS Style

    Qian Wendao; Yin Taiju; Sun Shaochuan; Zhang Changmin; Hou Guowei, et al. Identification of Diagenetic Facies Based on Diagenetic Process: An Example from Paleogene Lake Sediment Sandstone in Bozhong X Oilfield. Earth Sci. 2018, 7(4), 158-165. doi: 10.11648/j.earth.20180704.13

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    AMA Style

    Qian Wendao, Yin Taiju, Sun Shaochuan, Zhang Changmin, Hou Guowei, et al. Identification of Diagenetic Facies Based on Diagenetic Process: An Example from Paleogene Lake Sediment Sandstone in Bozhong X Oilfield. Earth Sci. 2018;7(4):158-165. doi: 10.11648/j.earth.20180704.13

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  • @article{10.11648/j.earth.20180704.13,
      author = {Qian Wendao and Yin Taiju and Sun Shaochuan and Zhang Changmin and Hou Guowei and He Miao and Xia Min},
      title = {Identification of Diagenetic Facies Based on Diagenetic Process: An Example from Paleogene Lake Sediment Sandstone in Bozhong X Oilfield},
      journal = {Earth Sciences},
      volume = {7},
      number = {4},
      pages = {158-165},
      doi = {10.11648/j.earth.20180704.13},
      url = {https://doi.org/10.11648/j.earth.20180704.13},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20180704.13},
      abstract = {Based on diagenetic evolution, reservoir diagenetic facies evolution was restored in burial history through quantitatively calculating the original porosity reconstructed by compaction, cementation and dissolution using core measurement data. The essence of this method was illustrated and its effectiveness was demonstrated using Paleogene lake sediment sandstone in Bozhong X oilfield, Bohai Bay Basin, China. Because diagenetic field changes as the structure depth increases or decreases and acts on deposition, diagenetic facies can be significantly different in different geological period. The Ed1 reservoir has experienced such an evolutionary process of W-Com_W-Cla-C_M-Car-C to M-Com_M-Clay-C_W-Qua-C_W-Fel-D_W-Car-D to M-Com_M-Cla-C_W-Qua-C_W-Fel-D_W-Car-D, while the Ed2 , the Ed3 and the Es1  are W-Com_W-Cla-C to M-Com_M-Cla-C-S-Com_S-Clay-C_W-Qua-C_W-Fel-D to S-Com_S-Cla-C_W-Qua-C_M-Fel-D, M-Com_W-Cla-C_W-Qua-C_W-Fel-D to M-Com_M-Cla-C_W-Qua-C_W-Fel-D to S-Com_M-Clay-C_W-Qua-C_S-Fel-D to S-Com_S-Clay-C_M-Qua-C_S-Fel-D and M-Com_W-Cla-C_W-Car-C to M-Com_M-Cla-C_W-Car-C_M-Fel-D_W-Car-D to M-Com_M-Clay-C_S-Fel-D_M-Car-D to S-Com_M-Cla-C _S-Fel-D_ M-Car-D respectively. Through this study, the reason for the dynamic change of sand body in the diagenetic field and the anisotropy of the reservoir are revealed.},
     year = {2018}
    }
    

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  • TY  - JOUR
    T1  - Identification of Diagenetic Facies Based on Diagenetic Process: An Example from Paleogene Lake Sediment Sandstone in Bozhong X Oilfield
    AU  - Qian Wendao
    AU  - Yin Taiju
    AU  - Sun Shaochuan
    AU  - Zhang Changmin
    AU  - Hou Guowei
    AU  - He Miao
    AU  - Xia Min
    Y1  - 2018/07/07
    PY  - 2018
    N1  - https://doi.org/10.11648/j.earth.20180704.13
    DO  - 10.11648/j.earth.20180704.13
    T2  - Earth Sciences
    JF  - Earth Sciences
    JO  - Earth Sciences
    SP  - 158
    EP  - 165
    PB  - Science Publishing Group
    SN  - 2328-5982
    UR  - https://doi.org/10.11648/j.earth.20180704.13
    AB  - Based on diagenetic evolution, reservoir diagenetic facies evolution was restored in burial history through quantitatively calculating the original porosity reconstructed by compaction, cementation and dissolution using core measurement data. The essence of this method was illustrated and its effectiveness was demonstrated using Paleogene lake sediment sandstone in Bozhong X oilfield, Bohai Bay Basin, China. Because diagenetic field changes as the structure depth increases or decreases and acts on deposition, diagenetic facies can be significantly different in different geological period. The Ed1 reservoir has experienced such an evolutionary process of W-Com_W-Cla-C_M-Car-C to M-Com_M-Clay-C_W-Qua-C_W-Fel-D_W-Car-D to M-Com_M-Cla-C_W-Qua-C_W-Fel-D_W-Car-D, while the Ed2 , the Ed3 and the Es1  are W-Com_W-Cla-C to M-Com_M-Cla-C-S-Com_S-Clay-C_W-Qua-C_W-Fel-D to S-Com_S-Cla-C_W-Qua-C_M-Fel-D, M-Com_W-Cla-C_W-Qua-C_W-Fel-D to M-Com_M-Cla-C_W-Qua-C_W-Fel-D to S-Com_M-Clay-C_W-Qua-C_S-Fel-D to S-Com_S-Clay-C_M-Qua-C_S-Fel-D and M-Com_W-Cla-C_W-Car-C to M-Com_M-Cla-C_W-Car-C_M-Fel-D_W-Car-D to M-Com_M-Clay-C_S-Fel-D_M-Car-D to S-Com_M-Cla-C _S-Fel-D_ M-Car-D respectively. Through this study, the reason for the dynamic change of sand body in the diagenetic field and the anisotropy of the reservoir are revealed.
    VL  - 7
    IS  - 4
    ER  - 

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Author Information
  • School of Geoscience of Yangtze University, Wuhan, China

  • School of Geoscience of Yangtze University, Wuhan, China

  • Zhongyuan Oilfield of Sinopec, Puyang, China

  • School of Geoscience of Yangtze University, Wuhan, China

  • Shanghai Branch of CNOOC Ltd., Shanghai, China

  • Shanghai Branch of CNOOC Ltd., Shanghai, China

  • School of Geoscience of Yangtze University, Wuhan, China

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