川东北复杂构造背景下致密砂岩裂缝发育模式与控产作用

    Fractures development pattern and the differential productivity-controlling of the fractures in tight sandstone under complex structural background, northeastern Sichuan Basin

    • 摘要:
      研究目的 为厘清川东北复杂构造背景下致密砂岩裂缝的发育模式与差异控产机制,提升天然气勘探开发效率,有必要深化裂缝研究。
      研究方法 基于二维和三维地震资料精细解释,结合野外露头观测、岩心描述、成像测井解释及产能分析,在构造演化特征系统研究的基础上,分区带明确裂缝特征及其空间差异,进而分析裂缝发育主控因素及其对产能的控制作用。
      研究结果 研究表明:①川东北须家河组先后经历燕山早中期、燕山晚期及喜马拉雅期3期构造变形,构造样式复杂,依据变形特征将研究区划分为5个构造区带;②NE向弱构造变形区及川东高陡构造带以低角度裂缝和平缝为主,裂缝开度小;其他区带中、高角度裂缝较发育,开度大;通南巴背斜与NE向弱变形区张性裂缝较多,但多数为不完全充填裂缝,其他地区剪切缝占主导,部分裂缝未充填;③裂缝发育程度受控于3期构造叠加作用、断褶构造组合样式与岩性及其组合特征,自西向东构造裂缝发育程度逐渐增强;且NW向断层成因裂缝对产能提升作用显著,裂缝发育程度与产量呈正相关。
      结论 NW向晚期断层成因裂缝对致密砂岩气藏产能具关键性控制作用,应作为下一步勘探开发的重要目标。

       

      Abstract:
      Objective This study aims to clarify the fracture development pattern and differential productivity−controlling mechanisms of the fractures in Xujiahe Formation tight sandstone under the complex structural background in the northeastern Sichuan Basin. The goal is to enhance the efficiency of natural gas exploration and development and improve single−well productivity in the region.
      Methods Based on detailed interpretation of 2D seismic and 3D seismic data of Sinopec Exploration areas, the structural characteristics and evolution of the Xujiahe Formation was investigated. The characteristics and spatial variation of fractures are identified through field outcrop observations, core description, borehole imaging interpretation, and production analysis. And the main controlling factors of fracture development and their impact on reservoir productivity are further analyzed.
      Results The findings indicate that: ① The Xujiahe Formation in the northeastern Sichuan Basin experienced three stages of tectonic deformation during the early−middle Yanshanian, late Yanshanian, and Himalayan period. Based on deformation styles, the study area is divided into five tectonic zones. ② NE−trending Weak Deformation Zone and Steep Structural Zone are dominated by low−angle and bedding−parallel fractures with small apertures, whereas high− and medium−angle fractures with wider apertures are more developed in other zones. Tensile fractures are well developed in Tongnanba Anticline and NE−trending Weak Deformation Zone, although many are significantly filled. Shear fractures dominate in other zones, and most are unfilled or only partially filled. ③ Fracture development is jointly controlled by three−stage tectonic superposition, structural styles, and lithological assemblages. From west to east, fractures increase progressively. NW−trending fault−related fractures have a significant positive impact on well productivity, and fracture development shows a positive correlation with production.
      Conclusions Late−stage NW−trending faults and their associated fractures play a key role in controlling productivity of tight sandstone gas reservoirs and should be considered favorable targets for future exploration and development.

       

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