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    中国百强科技报刊

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    Volume 46 Issue 9
    Oct.  2021
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    Article Contents
    Zhang Li, Shu Zhiguo, He Sheng, Chen Miankun, Wu Ningnan, Yang Rui, 2021. Reservoir Characteristics and Differential Evolution Process of Xujiahe Formation in Jiannan Area, East Sichuan. Earth Science, 46(9): 3139-3156. doi: 10.3799/dqkx.2020.302
    Citation: Zhang Li, Shu Zhiguo, He Sheng, Chen Miankun, Wu Ningnan, Yang Rui, 2021. Reservoir Characteristics and Differential Evolution Process of Xujiahe Formation in Jiannan Area, East Sichuan. Earth Science, 46(9): 3139-3156. doi: 10.3799/dqkx.2020.302

    Reservoir Characteristics and Differential Evolution Process of Xujiahe Formation in Jiannan Area, East Sichuan

    doi: 10.3799/dqkx.2020.302
    • Received Date: 2020-08-21
      Available Online: 2021-10-14
    • Publish Date: 2021-10-14
    • The reservoir of Xujiahe Formation in the Jiannan area of East Sichuan basin is highly heterogeneous and the densification is extremely high. To clarify the process and the controlling factors of reservoir differential evolution, a variety of experimental methods of petrology and petrogeochemistry are used in this study. Based on the detailed description for petrology characteristics of the reservoir, the diagenetic facies are classified; then the rock properties and pore structures are characterized, and finally the reservoir differential evolution process is investigated. Sandstones in study area can be divided into four diagenetic facies, namely, tight compaction facies, dissolution facies, siliceous cementation facies and tight calcite cementation facies. Sandstones from dissolution facies have the best rock properties, followed by the tight compaction sandstone. Siliceous cementation sandstone and calcite cementation sandstone are highly densified with the poorest rock properties. The variations of detrital component are the key factors controlling the heterogeneity and differential evolution of the reservoir. The various contents of ductile rock fragments result in the different degrees of compaction and pore reduction in the early diagenetic period, while feldspar and quartz contents affect the dissolution and calcite cementation degree, and the siliceous cementation degree, respectively. Finally, the detrital component controls the evolution process of reservoir in a different time order, and results in the spatial heterogeneity for the distribution.

       

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