通过野外地质调查、剖面实测、页岩气调查井(ZY3井)资料采集和样品测试,分析了芦草沟组沉积相、岩相特征,从矿物组成、孔渗特征和岩石力学参数等角度研究了芦草沟组页岩储层特征及主要储集空间类型,并探讨了其影响因素。结果显示:芦草沟组页岩储层整体呈特低孔(平均值0.98%)、特低渗(平均值0.04mD,1mD≈0.987×10-3μm2)的特征;微观孔隙以连通性、吸附性较差的微米级基质粒间孔为主,主要储集空间类型为裂缝和微裂缝,气体多以游离态赋存;页岩样品的柏松比(平均值0.22)与杨氏弹性模量(平均值1.34×104MPa)交会图以及高脆性矿物含量(平均值66.98%)均指示其具有良好的可压裂性和天然裂缝发育条件。认为芦草沟组页岩储层发育主要受沉积环境、矿物组成和成岩作用影响。
In order to analyze the characteristics of the lithofacies and sedimentary facies of the Lucaogou Formation,we investigated a number of samples collected from the well drilling ZY3 and from the outcrop in the field.Furthermore,we analyzed the mineral composition,porosimetry and permeability,microstructure of pores and fractures,and mechanical parameters of the rock,and we discussed the factors influencing them.The shale reservoir in the Lucaogou Formation exhibits ultra-low porosity (0.98% in average) and permeability (004mD in average).The microporosity is mostly constituted by matrix intergranular pores at μm scale,which confer poor connectivity and adsorption capacity.The main types of reservoir spaces are the cracks and microcracks,where the shale gas can be reserved in dissociated state.The cross-plot of the Poissons ratio (0.22 in average) and Youngs modulus (1.34 × 104MPa in average),as well as the content of brittle minerals (66.98% in average),suggest that the shale reservoir in the Lucaogou Formation has a high degree of brittleness and offers favorable conditions for natural fracture development.The development of the shale reservoir in the Lucaogou Formation is mainly influenced by the sedimentary environment,mineral composition,and diagenesis.
新疆维吾尔自治区地勘基金项目“新疆准噶尔盆地南缘重点远景区页岩气调查评价”(N13-4-XJ02)资助。