机构地区:[1]中国石化西北油田分公司勘探开发研究院,新疆乌鲁木齐830011 [2]中国地质科学院地质力学研究所,北京100081
出 处:《地质力学学报》2024年第3期394-407,共14页Journal of Geomechanics
基 金:中国博士后科学基金项目(2018M631541);中国地质调查局地质调查项目(DD20221660-1,DD20242777)。
摘 要:地质力学分析在油气藏勘探开发过程中发挥着重要作用,顺北油气田中—下奥陶统一间房组—鹰山组储层地应力研究相对滞后。对比分析了顺北4号带下古生界中—下奥陶统一间房组—鹰山组碳酸盐岩不同类型储层的岩石力学和地应力特征,同时探讨了微观颗粒结构对碳酸盐岩储层地应力和岩石力学参数的控制作用,为顺北地区超深层碳酸盐岩储层评价提供了基础地质依据。基于弹簧组合模型,通过岩石力学实验和阵列声波测井确定了岩石力学和地应力特征,通过铸体薄片和X射线CT扫描表征碳酸盐岩的微观孔隙结构。研究结果表明:顺北4号带一间房组—鹰山组杨氏模量分布在50~89 GPa,抗压强度在99~136 MPa,泊松比在0.25~0.32;地层最大水平主应力为200~225 MPa,最小水平主应力为125~160 MPa。一间房组—鹰山组碳酸盐岩不同类型储层的岩石力学参数和地应力存在明显差异,从Ⅰ类、Ⅱ类、Ⅲ类到非储层段碳酸盐岩的杨氏模量、抗压强度和最大水平主应力明显增大,而泊松比和最小水平主应力变化不大。相比于一间房组—鹰山组泥晶灰岩,砂屑-生屑灰岩方解石颗粒较大,颗粒黏结程度降低,导致岩石抗压强度和杨氏模量减小;砂屑-生屑灰岩部分方解石颗粒呈次圆状或圆状,颗粒三维空间球度较大,颗粒之间咬合作用减弱,使得岩石的抗压强度和杨氏模量减小;砂屑-生屑灰岩存在大量的孔隙和裂缝,灰岩易沿着潜在的微裂缝面或者颗粒接触面摩擦滑动甚至破裂,同样导致岩石抗压强度和杨氏模量减小。此外,一间房组—鹰山组泥晶灰岩受热液作用影响,部分白云石交代为石英,导致泥晶灰岩的抗压强度和杨氏模量增加。岩石的宏观力学特征和岩石力学参数受岩石微观颗粒结构的制约,一间房组—鹰山组杨氏模量、抗压强度和最大水平主应力低值区即为顺北4号带优势储层发育�[Objective]Geomechanical analysis plays a crucial role in exploring and developing oil and gas reservoirs.However,the study of in-situ stress in the Yijianfang–Yingshan formations of the Middle to Lower Ordovician in the Shunbei oilfield has lagged behind.This paper compares and analyzes the rock mechanics and in-situ stress characteristics of different types of carbonate reservoirs in the Yijianfang-Yingshan formations of the Lower Paleozoic Ordovician in the Shunbei No.4 block,and explores the control effect of micro-grain structures on the in-situ stress and rock mechanics parameters of carbonate reservoirs.It aims to provide fundamental geological data for the evaluating of ultra-deep carbonate reservoirs in the Shunbei area.[Methods]This study,based on the spring combination model,determined the rock mechanics and in-situ stress characteristics through rock mechanics experiments and array acoustic logging,and characterized the micro-pore structure of the limestone using casting thin sections and X-rayμ-computed tomography analysis.[Results]The results indicate that the Young's modulus of the Yijianfang–Yingshan formations ranges from 50 to 89 GPa,the compressive strength from 99 to 136 MPa,and the Poisson's ratio from 0.25 to 0.32.The maximum horizontal principal stress of the formations ranges from 200 to 225 MPa,while the minimum horizontal principal stress ranges from 125 to 160 MPa.[Conclusion]Significant differences in rock mechanics parameters and insitu stress exist among different types of carbonate reservoirs in the Yijianfang–Yingshan formations.From Type I to Type III and non-reservoir carbonate rocks,the Young's modulus,compressive strength,and maximum horizontal principal stress increase dramatically,while the Poisson's ratio and minimum horizontal principal stress show little change.Compared to micritic limestone,sandy–bioclastic limestone has larger calcite particles and reduced particle cohesion,resulting in decreased compressive strength and Young's modulus.Some calcite particles ap
分 类 号:P634.1[天文地球—地质矿产勘探]
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