Lithologic characteristics and reservoir evolution of tight sandstones in the upper Triassic Xujiahe formation, northeast Sichuan Basin, China

Jianbo Gao , Ningliang Sun , Bing Hao , Jianhua Zhong , Zhiwei Chen , Zhifeng Cao
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Abstract

The Xujiahe Formation sandstones in the northeast Sichuan Basin are an important tight gas reservoir. Mineralogical, petrographic, and geochemical data were used to constrain the diagenesis and evolution of the reservoir quality. The Xujiahe sandstones are mainly classified as litharenite and feldspathic litharenite (lithofacies 1) and sublitharenite and quartz arenite (lithofacies 2). The clay mineral is dominated by illite and mixed-layer illite/smectite. The reservoir quality is poor, with a porosity of 0.1–5.6 % (average of 1.7 %) and permeability between 0.006–2.83 × 10−3 μm2 (average of 0.05 × 10−3 μm2). Sandstones develop a nanopore network with a strong heterogeneous pore structure and poor throat sorting. Intercrystalline micropores and microfractures are favorable pore types. The sandstones underwent significant diagenetic alterations and were dominated by mechanical compaction, volcanic ash alteration, authigenic clay minerals transformation, quartz and carbonate cementation, feldspar and rock fragment dissolution, and pressure dissolution. The diagenetic evolution enters the Telodiagenesis stage. The homogenization temperature (Th) of fluid inclusions within the calcite cement of lithofacies 1 is 102.7–198.2 °C, whereas it is 159.3–205.6 °C for lithofacies 2, indicating that lithofacies 1 experienced additional stages of carbonate cementation. The Th within quartz cement has high values. Lithofacies 1 is 102.4–209.7 °C, whereas lithofacies 2 is between 145.7 and 207.7 °C, indicating that pressure dissolution significantly decreased pore spaces in the late diagenetic stage. Depositional and diagenetic factors controlled reservoir quality. Good grain sorting and relatively big grain size are available for primary pore protection, whereas cementation evidently destroyed reservoir quality. Reservoir and porosity evolution processes indicate that lithofacies 2 has relatively good porosity. This study successfully improves the exploration and development efficiency of Xujiahe tight sandstone gas and can be applied to similar gas fields worldwide.

Abstract Image

四川盆地东北部上三叠统须家河组致密砂岩岩性特征及储层演化
川东北须家河组砂岩是重要的致密气藏。利用矿物学、岩相学和地球化学资料对储层物性的成岩演化进行了约束。须家河砂岩主要分为岩屑岩和长石岩屑岩(岩相1)和亚岩屑岩和石英岩屑岩(岩相2),粘土矿物以伊利石和混层伊利石/蒙脱石为主。储层质量较差,孔隙度为0.1 ~ 5.6%(平均1.7%),渗透率为0.006 ~ 2.83 × 10−3 μm2(平均0.05 × 10−3 μm2)。砂岩形成的纳米孔网络具有较强的非均质孔隙结构和较差的喉道分选。晶间微孔和微裂缝是有利的孔隙类型。砂岩经历了明显的成岩蚀变,主要表现为机械压实作用、火山灰蚀变作用、自生粘土矿物转化作用、石英和碳酸盐胶结作用、长石和岩屑溶蚀作用以及压力溶蚀作用。成岩演化进入晚期成岩阶段。岩相1方解石胶结体流体包裹体均一温度(Th)为102.7 ~ 198.2℃,而岩相2流体包裹体均一温度(Th)为159.3 ~ 205.6℃,表明岩相1经历了额外阶段的碳酸盐胶结作用。石英胶结物中的Th值较高。岩相1为102.4 ~ 209.7℃,岩相2为145.7 ~ 207.7℃,表明成岩晚期压力溶蚀作用使孔隙空间明显减小。沉积和成岩因素控制着储层质量。良好的颗粒分选和较大的粒度对孔隙具有初级保护作用,胶结作用对储层质量破坏明显。储层和孔隙演化过程表明,2岩相具有较好的孔隙度。该研究成功地提高了须家河致密砂岩气的勘探开发效率,可应用于全球同类气田。
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