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    英买34、35井区志留系柯坪塔格组储层特征及其控制因素

    Reservoir characteristics and controlling factors of Silurian Kepingtage Formation in YM34 and YM35 well blocks

    • 摘要: 提要:志留系柯坪塔格组海相砂岩是英买力地区的主要储层和产层。英买力34、35两个井区的储层岩性、沉积环境均十分相似,而储层物性相差很大。通过储层岩石学、孔隙类型和孔隙结构、储层物性、成岩作用等多种特征综合研究,认为英买34、35区储层同为无障壁滨浅海沉积石英砂岩。英买34井区储层物性较好,属于中孔、中渗储层;英买35井区储层基质物性很差,属于特低孔、特低渗储层,但是张性微细裂缝发育,属于孔隙-裂缝复合型储层。试油结果表明两个区均具有较高产能且比较稳定。在充分认识两个区储层特征的基础上,笔者认为英买34、35井区储层性质的差异是后生成岩作用和构造作用造成的。

       

      Abstract: Abstract:Silurian seashore sandstone is the main oil reservoir and oil-producing formation in YM34 and YM35 well blocks. The lithology and depositional setting of these two well blocks are very similar to each other, but their reservoir properties are different significantly. According to such characteristics of these two blocks as lithology, porous styles, porous architectures, physical properties and diagenesis, the reservoirs of both YM34 and 35 well blocks are composed of seashore silicarenite in no-barrier shoreland. The YM34 well block is of moderate porosity and permeability, while the YM35 well block is of extremely low porosity and permeability, with the reservoir matrix properties of the former better than those of the latter. Nevertheless, the open fractures are developed significantly in the YM35 well block, suggesting a porous fractured complex reservoir. Well test shows that both the well blocks are of high and stable deliverability. Based on the full understanding of the reservoir properties, this paper has reached the conclusion that diagenesis and tectonic activity are the main factors responsible for the differences of reservoir properties between the YM34 well block and the YM35 well block.

       

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