Characteristics and exploration targets of Chang 7 shale oil in Triassic Yanchang Formation, Ordos Basin, NW China

The geological characteristics and enrichment laws of the shale oil in the third submember of the seventh member of Triassic Yanchang Formation(Chang 7_(3)) in the Ordos Basin were analyzed by using the information of core observations, experiments and logging, and then the exploration potential and orientation of the Chang 7_(3) shale oil were discussed. The research findings are obtained in three aspects. First, two types of shale oil, i.e. migratory-retained and retained, are recognized in Chang 7_(3). The former is slightly better than the latter in quality. The migratory-retained shale oil reservoir is featured with the frequent interbedding and overlapping of silty-sandy laminae caused by sandy debris flow and low-density turbidity current and semi-deep-deep lacustrine organic-rich shale laminae. The retained shale oil reservoir is composed of black shale with frequent occurrence of bedding and micro-laminae. Second, high-quality source rocks provide a large quantity of hydrocarbon-rich high-quality fluids with high potential energy. The source-reservoir pressure difference provides power for oil accumulation in thin interbeds of organic-poor sandstones with good seepage conditions and in felsic lamina, tuffaceous lamina and bedding fractures in shales. Hydrocarbon generation-induced fractures, bedding fractures and microfractures provide high-speed pathways for oil micro-migration. Frequent sandstone interlayers and felsic laminae provide a good space for large-scale hydrocarbon accumulation, and also effectively improve the hydrocarbon movability. Third, sand-rich areas around the depression are the main targets for exploring migratory-retained shale oil. Mature deep depression areas are the main targets for exploring retained oil with medium to high maturity. Theoretical research and field application of in-situ conversion in low-mature deep depression areas are the main technical orientations for exploring retained shale oil with low to medium maturity.

Method of moderate water injection and its application in ultra-low permeability oil reservoirs of Yanchang Oilfield, NW China

To explore the method of improving development effect and solving the problem of water breakthrough and water out for ultralow permeability fractured reservoirs, an indoor evaluation method of dynamic imbibition for fracture-matrix system was established taking the Chang 8 reservoir in southern Yanchang Oilfield as a research target. Key factors for the imbibition effect were obtained, an imbibition's rate expression was obtained, a model considering the double effects of imbibition-displacement was built and optimal injection and production parameters for the research area were obtained as well. The results show that an optimum displacement rate that maximizes the oil displacement efficiency exists in the water displacing oil process, and the optimal displacing rate becomes smaller as the permeability decreases. The imbibition displacement efficiency increases as the reservoir quality index and water wettability index of rock become bigger. But the larger the initial water saturation or oil-water viscosity ratio is, the smaller the imbibition displacement efficiency is. The optimal injection-production ratio for the Chang 8 reservoir of southern Yanchang Oilfield is 0.95, and the predicted recovery is 17.2% when the water cut is 95%, it is 2.9% higher than the recovery of conventional injection-production ratio 1.2. By using the moderate water injection technique based on the double effects of imbibition-displacement mechanism, the water injection development effect for the ultra-low permeability fractured reservoirs can be improved significantly.

Features of Sandy Debris Flows of the Yanchang Formation in the Ordos Basin and Its Oil and Gas Exploration Significance

Sandy debris flow is a new genetic type of sand bodies,which has gained much attention in recent years and its corresponding theory is proved to be a significant improvement and even partial denial to the 'Bouma Sequence' and 'turbidite fan' deep-water sedimentary theories to some point. Oil exploration researchers are highly concerned with sandy debris flows for its key role in controlling oil and gas accumulation processes.In this article,by applying sandy debris flows theory and combining a lot work of core,outcrop observation and analysis plus seismic profile interpretation,we recognized three types of sedimentary gravity flows that are sandy debris flows,classic turbidites and slumping rocks in chang-6 member of Yanchang Formation in the deep-water area of central Ordos Basin.Among the three types,the sandy debris flows are the most prominent and possesses the best oil bearing conditions.On the contrary,the classic turbidites formed by turbidity currents are limited in distribution;therefore,previous Yanchang Formation deep-water sedimentary studies have exaggerated the importance of turbidite currents deposition.Further study showed that the area distribution of deep water gravity flow sand bodies in Yanchang Formation were controlled by the slope of the deep-water deposits and the flows had vast distribution,huge depth and prevalent advantages for oil forming,which make it one of the most favorable new areas for Ordos Basin prospecting.

Characteristics and Origin of Tight Oil Accumulations in the Upper Triassic Yanchang Formation of the Ordos Basin,North-Central China

The Upper Triassic oil accumulations in the Ordos Basin is the most successful tight oil play in China,with average porosity values of less than 10% and permeability values below 1.0 mD.This study investigated the geological characteristics and origin of the tight oil accumulations in the Chang 6 member of the Upper Triassic Yanchang Formation in the Shanbei area based on over 50,000 petrological,source-rock analysis,well logging and production data.The tight oil accumulation of the Chang 6 member is distributed continuously in the basin slope and the centre of the basin.The oilwater relationships are complex.Laumontite dissolution pores are the most important storage spaces,constituting 30%-60% of total porosity and showing a strong positive relationship with oil production.The pore-throat diameter is less than 1 μm,and the calculated critical height of the oil column is much larger than the tight sand thickness,suggesting that the buoyancy was probably of limited importance for oil migration.The pressure difference between the source rocks and sandstone reservoirs is inferred to have provided driving force for hydrocarbon migration.Two factors of source-reservoir configuration and laumontite dissolution contributed to the formation of the Chang 6 tight oil accumulations.Intense hydrocarbon generation and continuous sand bodies close to the hydrocarbon kitchen are the foundation for the large-scale oil distribution.Dissolution of feldspar-laumontite during the process of organic matter evolution generated abundant secondary pores and improved the reservoir quality.

Predicting the present-day in situ stress distribution within the Yanchang Formation Chang 7 shale oil reservoir of Ordos Basin, central China

The Yanchang Formation Chang 7 oil-bearing layer of the Ordos Basin is important in China for producing shale oil.The present-day in situ stress state is of practical implications for the exploration and development of shale oil;however,few studies are focused on stress distributions within the Chang 7 reservoir.In this study,the present-day in situ stress distribution within the Chang 7 reservoir was predicted using the combined spring model based on well logs and measured stress data.The results indicate that stress magnitudes increase with burial depth within the Chang 7 reservoir.Overall,the horizontal maximum principal stress(SHmax),horizontal minimum principal stress(Shmin) and vertical stress(Sv) follow the relationship of Sv≥SHmax>Shmin,indicating a dominant normal faulting stress regime within the Chang 7 reservoir of Ordos Basin.Laterally,high stress values are mainly distributed in the northwestern parts of the studied region,while low stress values are found in the southeastern parts.Factors influencing stress distributions are also analyzed.Stress magnitudes within the Chang 7 reservoir show a positive linear relationship with burial depth.A larger value of Young's modulus results in higher stress magnitudes,and the differential horizontal stress becomes higher when the rock Young's modulus grows larger.

Laminae combination and shale oil enrichment patterns of Chang 73 sub-member organic-rich shales in the Triassic Yanchang Formation, Ordos Basin, NW China

The Chang 73 sub-member of Triassic Yanchang Formation in the Ordos Basin was taken as an example and the lamina types and combinations,reservoir space features and shale oil enrichment patterns in organic-rich shale strata were investigated using core observation,thin section analysis,XRF element measurement,XRD analysis,SEM,high solution laser Raman spectroscopy analysis,and micro-FTIR spectroscopy analysis,etc.According to the mineral composition and thickness of the laminae,the Chang 73 organic-rich shales have four major types of laminae,tuff-rich lamina,organic-rich lamina,silt-grade feldspar-quartz lamina and clay lamina.They have two kinds of shale oil-bearing layers,"organic-rich lamina+silt-grade feldspar-quartz lamina"and"organic-rich lamina+tuff-rich lamina"layers.In the"organic-rich+silt-grade feldspar-quartz"laminae combination shale strata,oil was characterized by relative high maturation,and always filled in K-feldspar dissolution pores in the silt-grade feldspar-quartz laminae,forming oil generation,migration and accumulation process between laminae inside the organic shales.In the"organic-rich+tuff-rich lamina"binary laminae combination shale strata,however,the reservoir properties were poor in organic-rich shales,the oil maturation was relatively lower,and mainly accumulated in the intergranular pores of interbedded thin-layered sandstones.The oil generation,migration and accumulation mainly occurred between organic-rich shales and interbedded thin-layered sandstones.

Study on oil–source correlation by analyzing organic geochemistry characteristics: a case study of the Upper Triassic Yanchang Formation in the south of Ordos Basin, China

In the south of the Ordos Basin, the oil source of the Upper Triassic Yanchang Formation is confused all the time, which affects further exploration. In this study, oil sources from the oil layers of Ch6, Ch8 and Ch9 are all analyzed and confirmed. Through their carbon isotope value and biomarkers, characteristics of crude oils from the Yanchang Formation are analyzed. Then, the oil–source relation is discussed, with the source rocks' features.Finally, the oil–source relation is calculated through cluster analysis. It is believed that the oils from the Yanchang Formation deposit in a similar redox environment, with weak oxidation–weak reduction, and have all entered maturity stage. Ch9 crude oil is more mature than crude oils from Ch6 and Ch8, and has more advanced plants and fewer algae. Gas chromatography(GC) and gas chromatography–mass spectrometry(GC–MS) analysis show that crude oils from Ch6 and Ch8 may come from Ch7, and Ch9 crude oil may not. Cluster analysis displays that crude oils from Ch6 and Ch8 have closer squared Euclidean distance with Ch7 source rocks than Ch9 crude oil does,indicating crude oils from Ch6 and Ch8 stem from Ch7 source rocks. And Ch9 crude oil has rather close squared Euclidean distance with Ch9 source rocks, illustrating Ch9 crude oil may be from Ch9 source rocks. This research may provide the theoretical basis for the next exploration deploy in the south of Ordos Basin.

Geological characteristics and exploration of shale oil in Chang 7 Member of Triassic Yanchang Formation, Ordos Basin, NW China

A set of shale-dominated source rocks series were deposited during the heyday of lake basin development in the Member 7 of Triassic Yanchang Formation,Ordos Basin,and the thickness is about 110 m.Aimed at whether this layer can form large-scale oil enrichment of industrial value,comprehensive geological research and exploration practice have been carried out for years and obtained the following important geologic findings.Firstly,widely distributed black shale and dark mudstone with an average organic matter abundance of 13.81%and 3.74%,respectively,lay solid material foundation for the formation of shale oil.Secondly,sandy rocks sandwiched in thick organic-rich shale formations constitute an oil-rich"sweet spot",the average thickness of thin sandstone is 3.5 m.Thirdly,fine-grained sandstone and siltstone reservoirs have mainly small pores of 2–8μm and throats of 20–150 nm in radius,but with a large number of micro-pores and nano-throats,through fracturing,the reservoirs can provide good conductivity for the fluid in it.Fourthly,continued high-intensity hydrocarbon generation led to a pressure difference between the source rock and thin-layer reservoir of up to 8–16 MPa during geological history,driven by the high pressure,the oil charged into the reservoirs in large area,with oil saturation reaching more than 70%.Under the guidance of the above theory,in 2019,the Qingcheng Oilfield with geologic oil reserves of billion ton order was proved in the classⅠmulti-stage superimposed sandstone shale reservoir of Chang 7 Member by the Changqing Oilfield Branch through implementation of overall exploration and horizontal well volume fracturing.Two risk exploration horizontal wells were deployed for the classⅡthick layer mud shale interbedded with thin layers of silt-and fine-sandstones reservoir in the Chang 73 submember,and they were tested high yield oil flows of more than 100 tons per day,marking major breakthroughs in petroleum exploration in classⅠshale reservoirs.The new discoveries have expanded the domain of unconventional petroleum exploration.

鄂尔多斯盆地陆相页岩油藏天然裂缝刻画与储层改造对策

鄂尔多斯盆地陇东地区三叠系延长组长7段页岩油储层主要为深湖相泥页岩和重力流砂体的交互沉积,储层的分布在纵向和横向上均复杂多变,单砂体厚度薄,同时又受到天然裂缝的影响,对该区科学压裂、生产提出了一系列挑战,压窜、砂堵等工程问题与降本增产成为目前重要攻关方向。文章总结了近两年来针对该区天然裂缝刻画方面的工作和认识,以及在压裂改造方面的最新理念和对策。在综合地质研究的基础上,建立三维精细地质、油藏和地质力学模型,进行合理的压裂设计、施工、压裂后分析和计算机模拟,更好地了解天然裂缝和水力裂缝之间的相互作用和水力缝的扩展规律,达到定制化的压裂设计和施工优化。最终实现施工井与同平台邻井在产量相当的情况下,支撑剂的用量减少20%左右、压裂液用量减少10%左右。这种地质工程一体化工作流程使“一井一策”和“一段一法”真正落到实处,从长远来看,这将成为鄂尔多斯盆地陆相页岩油达到单井和井场EUR最佳效果的基础性技术保障。

致密油储层压裂裂缝扩展规律分析及影响研究

以鄂尔多斯延长组长7裂缝性致密油储层为例,开展致密油储层裂缝扩展实验研究,分析裂缝扩展的影响因素,并对裂缝扩展规律进行模拟分析,实验结果表明:长7致密油储层岩石杨氏模量、泊松比和抗压强度波动范围广,造成数值差异较大;矿物组成分布差异为3%~46%,平均值为16.85%左右;该区块储层岩石发育部分的天然裂缝,储层最大水平主应力和最小水平主应力差异较大,储层水平和垂直方向上的孔、渗、饱等物性差异较大。天然裂缝的形成和发展受自然裂缝存在与地应力场差异这两个关键因素的显著影响,长7储层原始状态下裂缝的形态呈现低角度。

鄂尔多斯盆地南缘华北探区页岩油储层岩石力学特性实验研究

针对鄂尔多斯盆地南部延长组7段页岩储层钻井过程中发生钻头适应性差和井壁垮塌等井下复杂状况,开展了岩石组构特征分析、力学特征分析和可钻性参数等力学特征分析。结果表明,鄂尔多斯盆地南缘页岩油储层中黏土以伊利石和伊/蒙混层为主,岩石结构及力学特性非均质性强。岩石表面层理结构明显,微裂缝和孔隙发育。页岩抗张强度为6.58~18.27 MPa,单轴抗压强度为76.79~169.29 MPa,高温下的内摩擦角为14.67°~36.71°,泊松比为0.167~0.352,主要集中在0.21附近,弹性模量为4 100~17 344 MPa。最小水平主应力梯度为1.89~2.14 MPa/100 m,最大水平主应力梯度为2.37~3.04 MPa/100 m,其中洛河地区最大、最小地应力梯度差值较大。地层可钻性级值为4.36~6.11,主要分布在5.5以下,属于软-中硬度地层,平均地层倾角小,在钻至水平段时,钻进方向与层理相同,与岩石接触面多互层,钻头磨损加重。基于页岩储层岩石力学特性认识,对于鄂南页岩油安全、高效地钻探具有指导意义。

泾河油田页岩油储层井壁失稳机理研究

针对鄂尔多斯盆地南部泾河油田延长组长7段页岩地层井壁失稳技术难题,开展了页岩矿物组分、微观结构及理化性能测试分析以揭示井壁失稳机理。结果表明,长7段页岩地层层理、裂缝发育,属于弱水敏硬脆性页岩,地层层理结构造成岩石弱结构面被破坏,黏土水化引起岩石结构强度降低,钻具机械扰动导致井壁失稳;同时,建立了页岩地层三压力剖面,理想钻井液密度为1.13 g/cm^(3),对于泾河油田页岩油“安全、高效、经济”钻探具有借鉴意义。

鄂尔多斯盆地西部古峰庄地区三叠系延长组裂缝特征及其对低渗透油藏的控制作用

[研究目的]鄂尔多斯盆地西部古峰庄地区三叠系延长组属于低渗透储层,天然裂缝较为发育,以往对裂缝特征研究较少,开展天然裂缝特征和形成时期研究对低渗透油藏勘探开发具有重要作用。[研究方法]文章通过野外露头、钻井岩心、成像测井、扫描电镜裂缝识别和流体包裹体、断裂活动、构造应力分析等方法展开了古峰庄地区延长组天然裂缝特征和控藏作用研究。[研究结果]延长组各段天然裂缝均发育,以长7段最为发育,其次为长8、长6段;裂缝以高角度裂缝和垂直裂缝为主,走向以NEE向为主,NE向次之,少量NW和NWW向;裂缝面可见方解石充填和明显过油痕迹。天然裂缝发育程度与岩层厚度、断裂活动密切相关。裂缝形成时期具有多期性,主要为燕山期和喜马拉雅期。[结论]延长组天然裂缝的发育改善了研究区低渗透储层的孔渗能力和储集空间,为低渗透油藏运移、储集和富集提供了良好条件,其发育程度与形成时期影响着低渗透油藏的成藏和产能。

鄂尔多斯盆地东南部长7段页岩油气富集主控因素

为明确鄂尔多斯盆地东南部长7段页岩油气富集主控因素,综合钻井、测井、岩心分析化验等资料,对研究区长7段页岩油气富集程度及其机理进行研究。页岩解析气量与烃源岩总有机碳含量呈正比,有机质含量控制页岩油气的总含量,有机质发育大量孔隙,页岩油气以吸附态和游离态赋存于有机孔隙中。储集层孔隙结构和孔隙度影响页岩油气的含量及赋存状态,吸附油气主要赋存于微孔中,游离油气主要赋存于中孔和大孔中,但中孔中游离气含量高于大孔,而孔隙度越大,页岩中油气绝对含量越高。砂岩夹层和富有机质页岩的配置关系控制着页岩油气的富集部位,根据粉砂岩、细砂岩与页岩的关系,延长组长7段页岩油气可划分为近源和源内2类,源内又可分为砂岩与页岩互层型、页岩夹砂岩型和页岩型;下伏于富有机质页岩中的砂体和透镜状砂体油气含量最高,其次是上覆于富有机质页岩的砂体和呈舌状或指状与富有机质页岩接触的砂体。

鄂尔多斯盆地延长组多油源贡献比例与分布规律:基于机器学习与可解释性研究

鄂尔多斯盆地延长组发育多套潜在的烃源岩,但不同烃源岩之间生物标志物特征相似,常规油源对比方法效果不佳,相关认识长期存在争议。基于这样的问题,本文提出了一种基于深度学习的油源对比方案,将人工智能方法应用于油源对比研究,所开展的工作和认识有:(1)以延长组不同层位大量泥岩、页岩样品的42种生物标志物参数作为学习数据,构建了一种识别未知样品油源类别的深度神经网络模型,对长7泥页岩、长8—长10泥页岩的判别正确率分别达到了79.6%和83.0%,实现了延长组主要烃源岩生烃产物的有效区分;(2)通过模型分析了大量砂岩、原油样品的油源分类,统计了不同烃源岩对于延长组各个油层组原油的贡献比例,总结了它们的分布规律;(3)基于目前较为先进的置换特征重要性(PFI)算法,对所得模型进行了敏感性分析,初步揭示了延长组两类主要烃源岩的生物标志物差异。本文对于人工智能方法、技术在石油分子地球化学领域的发展具有积极的参考价值。

鄂尔多斯盆地胡尖山地区长7段页岩型页岩油源储特征及勘探前景

鄂尔多斯盆地三叠系延长组长7段发育一套以富有机质泥页岩为主夹砂质沉积的烃源岩层系,其中长7段源内夹层型页岩油已取得勘探突破并实现规模效益开发,但页岩型页岩油前期研究相对较少,是否具有勘探开发前景还不够明确。为此,以长7段烃源岩为研究对象,开展基于岩心分析化验、测井资料解释的烃源岩源储特征评价和矿场开发试验,用以评价胡尖山地区长7段页岩型页岩油勘探前景。长7段岩心测试分析表明,页岩主要发育粒间孔、晶间孔及有机质孔,常见层理缝及有机质收缩缝,游离态轻质油主要赋存于粒间孔及页理缝;运用多溶剂连续分步抽提方法实验结果表明,长7段页岩中游离态轻质油比例可达到54.3%。通过地球化学特征分析,长7段页岩平均TOC为14.03%、平均生烃潜量为57.73mg/g,为优质烃源岩;有机质热演化程度较高,平均R_(o)为1.08%、平均T_(max)为450℃;岩石热解可动烃含量达到4.34mg/g,表明页岩型页岩油具有良好的资源基础。研究区长7段页岩有机质类型好、有机质含量高、岩石可压裂性好,盆地内直井试油试采表明页岩含油性较好,利用岩石热解法估算该地区页岩型页岩油可动烃资源量为4.1×10^(8)t,综合认为研究区页岩具有水平井体积压裂提产的勘探开发前景。

富县M区延长组长8资源潜力分析

富县M区自勘探以来,对长8油藏特征了解较少。为阐明其油藏分布规律,在大量资料与研究成果的基础上,对该区沉积微相、储层特征及油藏特征进行分析,预测油气勘探有利区,为该区的下步详细勘探与开发提供依据。

鄂尔多斯盆地合水地区三叠系长7段夹层型页岩油储层特征及主控因素

运用铸体薄片、扫描电镜、黏土矿物X射线衍射、电子探针、阴极发光、高压压汞、物性测试等资料,对鄂尔多斯盆地西南部合水地区三叠系延长组长7段夹层型页岩油储层特征及储层致密化主控因素进行了研究,建立了储层定量评价标准,并预测出有利储层分布。研究结果表明:(1)鄂尔多斯盆地合水地区三叠系长7段夹层型页岩油储层主要为岩屑长石砂岩与长石岩屑砂岩,成分成熟度低、填隙物含量高、孔喉结构复杂,具有高孔低渗特征。(2)胶结作用是研究区长7段夹层型页岩油储层致密化的主控因素,储层平均视胶结率为86.3%,达到强胶结程度,以自生黏土矿物中的伊利石胶结为主;压实作用对储层致密化起次要作用,储层平均视压实率为46.0%,为中等压实程度;溶蚀作用降低了储层的致密化程度,但储层渗流能力较低,酸性流体难以大规模溶蚀,平均视溶蚀率仅为13.8%,为弱溶蚀程度。(3)受中等压实—弱溶蚀—强胶结成岩作用的影响,储层非均质性较强,成岩系数差异较大。Ⅰ类储层成岩系数大于2.4,Ⅱ1类储层成岩系数为1.8~2.4,Ⅱ2类储层成岩系数为1.2~<1.8,Ⅲ类储层成岩系数小于1.2,Ⅰ类与Ⅱ1类储层为有利储层。区域上中部混源区有利储层发育规模最大,是勘探的主要目标区。

鄂尔多斯盆地陕北地区三叠系长7段致密油分布特征及控制因素

综合利用地球化学、扫描电镜、岩心薄片、测井等资料以及油井生产数据等,对鄂尔多斯盆地陕北地区三叠系延长组7段储层特征、烃源岩特征和致密油分布特征进行了分析,从烃源岩展布、输导体系和源-储组合关系3个方面对致密油差异富集控制因素进行了探讨,并总结了成藏模式。研究结果表明:(1)陕北地区长7段致密砂岩储层主要分布在一亚段(长71)和二亚段(长72),以灰色—灰白色长石砂岩和岩屑长石砂岩为主,长71和长72平均孔隙度分别为5.56%和7.32%,平均渗透率分别为0.097 m D和0.110 m D,长72储层物性更好;孔隙空间以溶孔为主,发育少量粒间孔。(2)研究区烃类主要来源于本地长72顶部和长73这2套烃源岩,平均厚度大于20 m,有机质丰度高,平均TOC值为3.02%,干酪根类型以Ⅰ型和Ⅱ1型为主,处于生烃高峰期,平均生烃量为270.2×10^(4)t/km^(2),长73烃源岩生烃潜力更大,供烃至长72储层,长71致密油来源于长72烃源岩;新安边地区三角洲前缘亚相末端的长72储层中致密油由湖盆烃源岩侧向供烃。(3)研究区致密油富集受烃源岩展布、砂体连通性以及源-储组合共同控制,在长72更富集,在新安边地区分布面积最大,安塞地区无大规模致密油聚集;纵向上和平面上致密油的聚集差异受控于烃源岩厚度和源-储组合关系,下生上储、上下生油而中间储集和砂泥互层时含油性更好;新安边地区三角洲前缘亚相末端的长72致密油聚集规模大于三角洲前缘主体,是由于三角洲前缘末端发育的局部连通砂体阻碍了湖盆烃类物质的侧向运移。(4)研究区致密油为“源控-砂控”成藏模式,远源河道优势砂体尖灭处和近源局部连通的砂体是有利勘探区。

延长油区富昌开发单元长2非均质性研究

以延长油区富昌开发单元长2储层为研究对象,依据岩心和测井资料从宏观和微观角度分别对长2储层非均质性进行了分析。研究结果表明:研究区长2段储层的渗透率在纵向剖面上以正韵律型为主、夹层类型以泥质夹层为主,层内非均质性整体较弱;三个小层分层系数都较低,隔层发育一般,具有中等层间非均质性;储层砂体及物性的平面展布特征受沉积相的影响而呈条带状分布,表现出较强平面非均质性;同时,孔喉类型多而且分选系数大,整体上微观非均质性较强。