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    断控栅状缝洞储集体影响下的碳酸盐岩储层地应力场表征以顺北4号断裂带为例

    Stress field characterization for carbonate reservoirs with fault-controlled grid-like fracture-cavity systems: A case study of Shunbei No. 4 fault zone

    • 摘要: 顺北油气田碳酸盐岩储层经历多期复杂构造运动,内部广泛发育由溶蚀孔洞与天然裂缝耦合形成的断控缝洞型储集体。此类储集体在空间上呈栅状分布,其内部裂缝与溶洞的组合模式对局部地应力场的分布及井漏演化机理具有显著控制作用。采用有限元数值模拟方法,建立了一种考虑裂缝和溶洞多尺度耦合效应、栅状储集体影响下的非均匀地应力场表征方法,并以顺北4号断裂带为例,基于SHB4-A井实际钻井、测井及储层结构数据,模拟分析了栅状储集体对储层局部地应力场分布的控制作用。研究结果表明:在以裂缝为主的储集体中,最小水平主应力升高而应力差减弱,整体处于高约束、低各向异性环境,井漏风险较低;在裂缝–溶洞连通条件下,溶洞的应力屏蔽作用使局部应力降低并保持高应力差,易沿裂缝形成导向性漏失通道;当裂缝与溶洞相邻但未连通时,在裂缝尖端与溶洞之间的部位会出现显著应力反转,极易发生瞬时贯通并诱发大规模井漏。

       

      Abstract: The carbonate reservoirs in Shunbei Oilfield, shaped by multi-phase complex tectonic movements, host widespread fault-controlled fracture-cavity systems characterized by dissolved pores and cavities coupled with natural fractures. The fracture-cavity configuration within these grid-like, fault-parallel reservoir systems controls both local stress field distribution and the dynamics of circulation loss. Based on a finite element numerical simulation model, we develop a characterization method for the heterogeneous stress field in fracture-cavity systems. This method accounts for the multi-scale coupling effects between fractures and cavities. Using the drilling, logging, and reservoir structure data from Well SHB4-A in the Shunbei No. 4 fault zone, we conduct numerical simulations to analyze the control of fracture-cavity systems on local stress distribution. The results show that within fracture-dominated zones, an increase in the minimum horizontal principal stress coupled with a decreased stress difference results in an environment of high confinement and low anisotropy, thereby reducing the risk of circulation loss. Under connected fracture–cavity conditions, the stress-shielding effect of cavities locally reduces horizontal stress while maintaining a high stress difference. This facilitates the formation of oriented leakage channels along the fractures. When fractures and cavities are adjacent but not connected, significant stress reversal occurs in the regions between the fracture tips and the cavities, leading to instantaneous hydraulic linkage and consequent large-scale circulation loss.

       

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