Tight Carbonate Microstructure and its Controls: A Case Study of Lower Jurassic Da'anzhai Member, Central Sichuan Basin

Cast thin section observation, scanning electron microscopy(SEM), high-pressure mercury injection(HPMI), and nuclear magnetic resonance(NMR) were used to examine the microstructure of tight carbonate reservoirs in the Lower Jurassic Da’anzhai Member, the central Sichuan Basin. The pore space in the Da’anzhai Member is classified into 2 types and 17 subtypes, with nano-scale pore throats of ‘O’, ‘S’, ‘Z’, and ‘I’ shapes. Poorly sorted pore throats vary greatly in diameter;thus, it is difficult for fluid flow to pass through these pore throats. There are three classes of pore throats in carbonate reservoirs, i.e. isolated pores, pores coexisting with fractures, and large pores and fractures. Isolated pores may provide some pore space, but the permeability is low. Pores and fractures coexisting in the reservoir may have a great impact on porosity and permeability;they are the major pore space in the reservoir. Large pores and fractures have a great impact on reservoir properties, but they only account for a limited proportion of total pore space. The microstructure of Da’anzhai reservoirs, which dominates fluid mobility, is dependent on sedimentary environment, diagenesis, and tectonic process. Pore structure is related to sedimentary environment. The occurrence of microfractures, which may improve reservoir properties, is dependent on tectonic process. Diageneses are of utmost importance to pore evolution, cementation and growth of minerals have played an important role in destroying reservoir microstructure.

Reservoir micro structure of Da'anzhai Member of Jurassic and its petroleum significance in Central Sichuan Basin, SW China

Based on the qualitative study of microscopic reservoir features using core analysis,cast and fluorescence thin sections inspection,scanning electron microscope(SEM)and field emission scanning electron microscope(FESEM)and quantitative examination of pore size and geometry using mercury injection,nano-CT and nitrogen adsorption,reservoir rock of Da’anzhai Member were divided into 9 types,while storage spaces were divided into 4 types and 14 sub-types.The study shows that sparry coquina is the most promising reservoir type.Pores that smaller than 1μm in diameter contribute 91.27%of storage space volume.Most of them exhibit slot-like geometry with good connectivity.By building up storage space models,it was revealed that micron scale storage spaces mainly composed of fractures and nanometer scale pores and fractures form multi-scale dual porosity system.Low resource abundance,small single well controlled reserve,and low production are related to the nano-scale pore space in Da’anzhai Memer,whereas the dual-porosity system composed of pores and fractures makes for long-term oil yield.Due to the existence of abundant slot-like pore space and fractures,economic tight oil production was achieved without stimulations.

Characteristics and significance of the penecontemporaneous karst in lacustrine carbonate, Da'anzhai Member, Lower Jurassic, Beibei area, eastern Sichuan Basin

There are few reports about the penecontemporaneous karst of the lacustrine carbonate of Da'anzhai Member which developed on the top of Lower Jurassic Ziliujing Formation,eastern Sichuan Basin.Based on the analysis of the macroscopic and microscopic characteristics of Heping Reservoir section in Beibei area,It is discovered that the penecontemporaneous karst in the lacustrine carbonate,Da'anzhai Member,and its characters as follows:(1)The dissolved fractures and karrens are common,which have been filled with vadose silts,bioclasts,terrigenous quartzes,crystal and intergrown calcites;(2)The penecontemporaneous karstification mainly occurs in the micrites and shell limestones of the middle and upper part of the shallowing-upward sequence,and the desiccation cracks occur in some shallowing-upward sequences;(3)Three meteoric-water diagenetic lenses are identified in this section.By further study we also find the factures,stylolite and burial dissolution pores occur along the karst system(tubes,conduits and caves of the karst).And the asphalt not only fills the stylolites and fractures,but also is mixed with the vadose silt in the karst system,although the pore space formed by penecontemporaneous karstification is filled with vadose material and cements.Therefore it is concluded that the development and modification of the tight lacustrine carbonate reservoir of Da'anzhai Member,to some extent,are relevant with the penecontemporaneous karstification,and the penecontemporaneous karst reservoir may develop in the buried Da'anzhai carbonate of the basin.

Reservoir and development characteristics of the Da'anzhai tight oil in Sichuan Basin,SW China

The oil in the Jurassic Da'anzhai reservoirs in the Sichuan Basin is unconventional tight oil,which accumulated in or near source rocks,and did not experience extensive migration in a large-scale long distance.The first submember,second submember and third submember of Da'anzhai Member are dominated by shell limestone which is widely and continuously distributed,and are typical near-source lacustrine shell limestone tight reservoirs.Complex lithology,multiple types of reservoir space and complicated pore structure are developed in these reservoirs.The effective reservoir space mainly includes micro-pores and micro-fractures with strong fabric selectivity.The petrophysics experiment reveals that the average connected matrix porosity of tight oil reservoir in Jurassic Da'anzhai Member is about 2.13%,lower than that of other tight oil reservoirs but higher than the average effective porosity(0.97%)from previous single alcohol-saturated method.According to production performance data,the Da'anzhai shell limestone reservoir is not a simple porous or fractured reservoir,but has complex porethroat-fracture association or storage-seepage mode.Because the development of fossil shells controls the development of micro-fractures,fluids are difficult to enter into but easy to escape from the reservoirs.Although the pore-throat is fine,the sorting is poor and the displacement pressure is high,the movable fluid saturation and mercury ejection efficiency of the reservoir in the Da'anzhai Member is only slightly lower than that of some storage-seepage modes,and higher than that of Oil-bearing Group 7 of Yanchang Formation in the Ordos Basin.The reservoir in the Da'anzhai Member is one of the few tight oil reservoirs with high natural productivity.The tight oil in the shell limestone of the Da'anzhai Member has great development potential,but its extensive and effective development also has some challenges,such as high seepage resistance of matrix and ineffective single development mode.The development mode of the Da'anzhai tight oil should draw lessons from the Bakken Formation in North America and Oil-bearing Gourp 7 of Yanchang Formation in the Ordos Basin,and thus,effective development technologies based on volume fracturing and fine operation for shell limestone tight oil in the Da'anzhai Member in Sichuan Basin are developed to realize the development of profit and scale.

川中—川东地区侏罗系大安寨段古环境及油气地质意义

【目的】四川盆地侏罗纪大安寨期不同地区古环境特征差异较大,探讨其演化特征及地质意义将有助于加快油气勘探的步伐。【方法】利用四川盆地中部和东部侏罗系大安寨段钻井岩心和野外剖面等地质资料,结合元素地球化学分析方法,对大安寨期古气候、古氧化还原、古盐度等古环境进行恢复和对比分析。【结果】川中—川东地区大安寨段岩性可划分为页岩、介壳页岩、泥岩、粉砂质泥岩、泥质粉砂岩、介壳灰岩和泥质介壳灰岩;大安寨第三亚段沉积期气候为干燥—半干燥,水体为亚还原条件的淡水—半咸水,处于浅湖—半深湖环境;大安寨第二亚段沉积期气候为半干燥—半潮湿,降水量较多,气温较低,水体为亚还原条件的淡水,处于半深湖环境;大安寨第一亚段沉积期气候为干燥—半干燥,水体为氧化—亚还原条件的半咸水—咸水,处于滨湖—浅湖环境;RA1井与YT1井大安寨时期均具有气候干燥→潮湿→干燥、降水量少→多→少、气温高→低→高、水体还原性弱→强→弱、古盐度高→低→高的规律;大安寨第三亚段沉积期至大安寨第二亚段沉积早期,湖盆沉积中心由川东地区往川中地区迁移,大安寨第二亚段沉积晚期至大安寨第一亚段沉积期,湖盆沉积中心则由川中地区往川东地区迁移;大安寨第二亚段TOC平均值为1.70%,孔隙度平均值为4.93%,荧光显示强烈,是大安寨段页岩油的主要生油层和储集层;古环境因素对源储配置具有较大影响,较潮湿的气候、较多的降水、较低的气温、还原性的水体和较低的盐度有利于泥页岩沉积、有机质富集和孔隙发育。【结论】川中—川东地区大安寨段古环境控制泥页岩沉积和有机质富集规律,影响页岩孔隙发育程度,这一认识可为明确四川盆地页岩油有利勘探区提供理论依据。

川中地区大安寨段页岩油储层孔隙微观形态研究

大安寨段湖相页岩是四川盆地页岩油勘探的关键层。为了解其微观孔隙,使用氩离子抛光、扫描电镜和图像处理软件提取高分辨率电镜图像的孔隙,获取不同孔隙的孔径、圆度、伸长率等参数。结果显示:大安寨段黑色页岩中有2类7种常见孔隙,主要是黏土孔隙、石英/方解石晶内孔隙、粒缘孔隙和有机孔;不同孔隙类型形态差异大,有机质孔隙小且凸性值趋近1,黏土晶间孔隙、粒缘孔隙圆度凸性值小、伸长率大,方解石晶内孔隙大且圆度凸性较大。孔隙大小和形状受组分和压实作用控制:无机孔隙普遍大于有机孔,无机孔中脆性矿物孔径最大,呈多边形,而塑性矿物孔径小,呈伸长率大的片状。

川东北地区大安寨段页岩油气资源评价与有利区优选

四川盆地是中国最具勘探潜力的非常规油气盆地之一,其中川东北地区的大安寨段地层发育富含机质并与薄层介壳灰岩互层的页岩,有生烃、含油含气的特征,具有页岩油气开发潜力。为明确四川盆地川东北地区大安寨段页岩储层的油气资源潜力,综合运用油气地球化学和地质学研究方法,对该地区的页岩油和页岩气的资源潜力进行评价,预测页岩油气的有利区。结果表明:大安寨段岩性主要为黑色页岩和介壳灰岩。其中,大二亚段为富含有机质的页岩层段;大安寨段累计厚度约为60~110m,埋藏深度约为1000~3600m;有机质类型以Ⅱ2型为主,有机碳含量介于0.42%~2.74%,平均值为1.18%;有机质成熟度为0.94%~1.84%,主要处于成熟—高成熟阶段;大安寨段页岩埋藏深度适中,有效厚度大,生烃潜力高,具备页岩油气成藏的基础条件;大安寨段页岩气和页岩油的有利区位于研究区西南部和东部,估算页岩气资源量为24543×10^(8)m^(3),页岩油资源量为10×10^(4)t。根据研究结果,分别优选研究区的页岩油气的Ⅰ类有利区带和Ⅱ类有利区带,可为大安寨段页岩油气勘探开发提供参考。

川中气田水回注大安寨段储层配伍性研究

为减少气田水对环境的影响,确保气田合理开发,目前对气田水最有效的处理方式是异层回注处理,但对不同气藏的气田水进行回注时,要保证回注成功和回注系统正常运行,必须进行配伍性实验。针对川中地区须家河组、嘉二段和长兴组气田水的水质特征,与回注层大安寨段地层水及岩心进行了配伍性实验,从而了解影响回注的因素,并提出相应的解决措施。在岩心伤害实验的基础上,推荐了气田地层水回注的水质指标。

四川盆地下侏罗统大安寨段页岩油气地质特征及勘探有利区优选

四川盆地下侏罗统大安寨段是页岩油气(致密油气)分布的主要层系之一,但由于钻探、测试效果均较差,急需开展有利层段地质特征和勘探有利区优选等研究工作。为此,利用野外露头、岩心、测录井及地球物理等资料研究了大安寨段页岩油气地质特征,分析了页岩油气富集的主控因素,并优选了勘探有利区。研究结果表明:①大安寨段为一套介壳石灰岩与黑色页岩的混积地层,页岩矿物类型以黏土为主,其次为石英、方解石,少量长石、黄铁矿,脆性矿物含量中等;②孔隙类型以无机孔隙为主,含少量有机孔,发育介壳壳缘缝、节理缝等多尺度裂缝,物性随介壳含量的增加而降低;③页岩有机质丰度为中等—好,TOC平均值为1.34%,有机质类型以混合型为主,少量腐泥型和腐殖型,R_(o)平均值为1.11%,热演化程度南低北高,整体处于成熟—高成熟阶段,含油性中等,氯仿沥青“A”含量平均为0.26%;④热解游离烃S1值平均为1.27 mg/g,OSI平均值为84.35 mg/g,页岩油气富集的烃源下限是TOC>1.5%,R_(o)>0.9%,纵向上排烃效率较低,含油指标较高段(OSI>100 mg/g)主要分布于厚层页岩中部;⑤可动油饱和度普遍小于20%,受纹理缝和页理缝影响,石灰岩—页岩互层型、页岩夹石灰岩型样品的油可动性好于石灰岩和页岩。结论认为,大安寨段页岩层系具有较好的页岩油气勘探开发潜力,高生烃品质、多尺度裂缝以及高地层压力是盆地页岩油气富集高产的关键因素,有利油气勘探区主要分布于川中地区三台—仪陇以及南充一带。

四川盆地侏罗系湖相页岩油气地质特征及勘探开发新认识

近年来,中石油、中石化、壳牌等国内外能源公司相继对四川盆地侏罗系自流井组大安寨段湖相页岩开展了油气勘探工作。为了有效地指导湖相页岩油气的相关勘探开发工作,针对该盆地侏罗系湖相油气资源量与储量不匹配、致密储层物性与油气产量不匹配等矛盾,综合岩心、露头、钻井、测井、试油、分析化验等资料,对侏罗系湖相油气系统开展了页岩油气地质特征、勘探开发对象等方面的研究工作。研究结果表明:①四川盆地侏罗系发育自流井组东岳庙段、大安寨段以及凉高山组上段共计3套优质页岩层系,具有源储一体、源储紧邻的特点,是典型的页岩油气发育层系,其中又以大安寨段为典型代表;②大安寨段页岩层系具有有机质含量高、有机质类型好、热演化程度适中、生烃能力强、页岩物性好、储集性能优、脆性矿物含量高、源储配置关系好、页岩厚度大、含油气性好等特征,是典型的页岩油气藏;③通过对大安寨段万吨井的解剖以及页岩有机质含量、热解参数、储层物性等试验数据揭示,该页岩油气藏存在着页岩与介壳灰岩两类储层的油气补给,并且前者的补给能力可能更强,故而页岩层系是侏罗系湖相页岩油气储量有效动用的主要对象;④基于目前的新认识,以页岩油气为勘探对象,通过非常规油气的技术手段,采用水平井+体积压裂技术,该层系一定会取得新的油气勘探突破。结论认为,该项研究成果可以为四川盆地侏罗系湖相页岩油气的资源发现以及储量有效动用等提供理论和技术支撑。

四川盆地侏罗系大安寨段湖相含云质储层成因研究

四川盆地侏罗系大安寨段是典型的致密油发育层段,勘探开发成果揭示,大安寨储层岩性主要为介壳灰岩致密储层。侏罗系大安寨段致密油勘探开发成效引人关注,特别是近期川中南部侏罗系大安寨段滨浅湖相的GSTMX地区,大安寨段显示频繁,部署的GQ1H在大安寨段获得高产工业油流。根据对最新钻探的GQ1H井解剖表明,含云质岩具有更好的储集条件和含油气性,是储层"甜点"有利分布岩性。通过老井复查、岩心、岩屑、薄片、测井等综合分析表明,含云质储层岩性包括云质灰岩、灰质云岩和泥-粉晶云岩,储集空间主要为粒间、粒间溶孔和微裂缝,储层储集条件好,成像显示溶蚀孔洞发育,川中南部云化程度高于北部。根据碳氧同位素、X衍射、地层水特征以及古地形综合分析初步认为,四川盆地大安寨沉积时期虽然为淡水湖泊,但在古地形、古气候、沉积环境以及湖平面变化共同控制下,局部地区仍然发育一定规模的含云质储层,该认识为川中侏罗系大安寨段相对优质储层深化认识奠定了坚实的地质基础。

四川元坝地区大安寨段陆相细粒沉积岩储层物性特征及有利储集层研究

四川盆地元坝地区大安寨段陆相细粒沉积岩不同于盆地内其他地区,储层的物性差异较大,需对该区域目的层段细粒沉积岩储层物性特征开展研究。综合利用薄片观察、氦气法测孔渗、低温氮气吸附、扫描电镜及FIB等方法,对研究区岩石的物性特征、储集空间、孔隙结构和渗透性进行分析研究。结果表明:研究区细粒沉积岩储层储集空间类型分为孔隙和裂缝两大类,包括有机质孔、粒间孔、溶蚀孔、晶间孔、黏土矿物间微孔和构造缝、页理缝、成岩收缩缝;平均孔隙度为3.35%,平均渗透率为1.54 mD,属于特低孔低渗的孔缝型储层;细粒岩储层以微孔和介孔为主,孔径主要为3~7 nm;大二亚段富有机质页岩和介壳页岩是最有利的储集岩性,大安寨段下部和中部的富有机质细粒岩段为有利储集层段。储层特征分析有助于揭示大安寨段陆相特低孔低渗致密储层形成机理,也可为该类储层成因解剖与分布规律预测提供支撑和借鉴。

川北下侏罗统自流井组大安寨段灰岩非常规储层包裹体研究

通过对川北大安寨段灰岩非常规储层流体包裹体的系统研究,表明该储层的成因与多期次的深部溶蚀作用有关,可划分为成岩期、构造期和构造期后3个溶蚀期及5个次生矿物沉淀阶段,各阶段流体包裹体类型、丰度、形态、均一温度、盐度、密度和成分特征各不相同,显示溶蚀流体来自油源岩区于不同演化阶段排出的无机和有机流体,因而包裹体的各项特征和演化规律可作为评价和预测大安寨段非常规储层的标志。

川北元坝地区大安寨段页岩微观孔隙空间定量表征

为了分析元坝地区大安寨段湖相页岩的天然气赋存特点,通过扫描电镜、氮气吸附、高压压汞等实验方法,研究了该区大安寨段页岩的孔隙类型与孔径分布,并探讨了页岩的孔隙结构对页岩气赋存状态的影响。结果表明:页岩中发育无机质孔隙(76.92%)、有机质孔隙(9.17%)与微裂缝(13.91%),其中无机质孔隙主要为蒙脱石伊利石化过程中形成的黏土矿物孔隙,有机质孔隙欠发育的原因与有机质类型以Ⅲ型为主且总有机碳含量低有关;页岩的全孔径分布中,微孔、中孔与宏孔分别贡献6.76%、76.92%与16.30%的孔体积。可见,元坝地区大安寨段页岩以无机孔为主,主要发育中-宏孔,与储层高温高压共同控制了该区页岩气的赋存方式以游离气为主。

湖相页岩水平井井壁稳定机理及钻井液安全密度窗口--以四川盆地侏罗系大安寨段为例

近期中石化、中石油相继在四川盆地侏罗系湖相页岩中取得了油气勘探突破,泰页1井、平安1井、龙安1井均在页岩段获得工业油气流,进一步展示了湖相页岩的油气勘探开发潜力。四川盆地湖相页岩是我国页岩油气勘探的重点方向,但页岩水平井井壁失稳风险较高,容易发生井壁坍塌、卡钻和埋钻事故,严重制约了水平井钻井提速提效和安全钻井。为了厘清湖相页岩的井壁稳定机理,以四川盆地侏罗系大安寨段湖相页岩为研究对象,系统开展了页岩矿物组成、微观结构、理化性能、岩石力学等测试分析,建立了钻井液安全密度窗口评价模型,分析了大安寨段页岩地层的井壁稳定性,并在N2H井验证了井壁稳定机理和钻井液安全密度窗口评价结果的准确性。研究结果表明:①大安寨段湖相页岩主要是应力集中过高、强度各向异性及钻井液穿透进入弱面造成的力学失稳,需要重视钻井液物理封堵性能;②直井和小角度定向井稳定性最好,井斜角超过45°后坍塌压力急剧增加;③沿最大水平地应力的水平井坍塌压力低、破裂压力高,井壁稳定性好,但不利于压裂;④沿最小水平地应力的水平井坍塌压力高、破裂压力低,井壁稳定性差,但有利于压裂。结论认为,N2H井安全密度窗口下限和上限分别为1.91~1.98 g/cm^(3)(均值为1.94 g/cm^(3))、2.37~2.55 g/cm^(3)(均值为2.45 g/cm^(3)),推荐油基钻井液密度介于2.05~2.30 g/cm^(3),预测结果与实钻情况吻合较好;该研究成果可以为大安寨段湖相页岩水平井井壁失稳防治、水平井钻井设计和施工提供有效的指导。

四川盆地侏罗系大安寨段湖相页岩油气形成地质条件及勘探方向

随着认识的不断深入和工程技术的进步,页岩油气已经正式进入我国储量序列,正在有序开发。通过岩心、露头、钻井、测井以及大量的分析化验资料,对四川盆地侏罗系大安寨段湖相页岩油气的形成地质条件和资源潜力进行系统分析和评价。研究结果表明:①大安寨段湖相页岩主要发育在大一三亚段浅湖、半深湖泥,有机碳含量平均为1.15%,有机质类型均以Ⅱ型干酪根为主,镜质体反射率介于0.8%~1.4%,处于成熟—高成熟阶段,页岩厚度大,生烃能力强,具备形成页岩油气的物质基础。②大安寨段页岩以黑色、灰黑色页岩与生物介壳灰岩不等厚互层为主,脆性矿物平均含量为63.4%含量较高;页岩孔隙度平均为5.92%,储集条件好,储层发育微米—纳米级孔隙,具备储集页岩油气的储集空间,有利于页岩储层的改造。③大安寨段湖相页岩油气具有埋藏浅、保存条件好、压力系数高等优越条件,按照有机碳含量大于1.5%的范围,计算页岩油资源量为70×10^8 t,页岩气的资源量为3.5×10^12 m^3,结合大安寨段页岩油气评价指标,优选出射洪—遂宁—南充—蓬安—仪陇—南部页岩油气勘探有利区近1×10^4 km^2,并建议在公山庙、龙岗地区开展先导试验工作。

层次分析法预测致密油甜点区的可行性——以川中侏罗系大安寨段为例

川中侏罗系大安寨段为典型自生自储致密油藏,储层物性差,纵向裂缝较发育,单井产量受多因素综合控制,无法用常规油藏勘探开发思维及已有行业评定标准进行分析。通过对川中侏罗系大安寨段进行研究,结合《SYT6943–2013致密油地质评价方法》,运用层次分析法预测川中侏罗系大安寨段致密油甜点区,并和当前掌握的地质情况与开采情况对比。研究表明:使用层次分析法可将模糊定性的地质结论量化为科学权重,有效解决了因地质资料不足而造成的分析瓶颈,降低了勘探风险;但致密油属非常规油藏,与常规油藏差别大,评估时各参数并不是越高或者越低越好的线性关系,而是需要找出参数区间或者上下限;层次分析法需与行业标准结合运用才能提高运算精度。

油层含油性判别分析

大安寨油组是川中油田的主力产油层 ,油气多产于碳酸盐岩地层 ,开采时间较长 ,不少井产量下降 ,甚至枯竭 ,因而研究大安寨油井含油特征、预测产能是十分必要的。根据试油井段的产能分析 ,将储层分为干层、低产层和高产层三类 ;应用测井、地质及试油试采资料 ,归纳出不同类型产层的定性特征 ;并建立起判别产层的模型 ,形成一套选取产层和预测产能的方法。

川西坳陷中江斜坡大安寨段陆相页岩油气地质特征

近年来,中国石化西南油气分公司在川西坳陷中江斜坡侏罗系自流井组大安寨段湖相层系加大勘探力度,多口井取得了工业油气流,展示了该区该层系良好的油气勘探潜力。为了进一步明确研究区侏罗系大安寨段页岩油气资源潜力,主要以陆相页岩油气形成地质特征为研究对象,分析了川西坳陷中江斜坡侏罗系自流井组大安寨段页岩沉积背景及平面展布特征,页岩有机碳含量及平面展布、有机质类型、有机质成熟度等页岩地球化学特征,页岩储层特征,页岩含气量特征,页岩油气保存条件和页岩工程物理特征,指出了川西坳陷中江斜坡侏罗系自流井组大安寨段具有良好的页岩油气形成地质条件。研究结果表明:①研究区大安寨段优质页岩具有厚度大、平面展布广、有机碳含量较高、有机质类型及有机质成熟度较好、物性较好、脆性矿物含量高的特征;②研究区大安寨段具有埋藏深度浅、地层压力系数高的特征,具备良好的工程改造条件。结论认为,研究区东部—东南部的福兴、回龙场、永太地区为页岩油气有利目标区,具备页岩油气勘探潜力。

元坝地区大安寨段二亚段页岩气储层孔隙度计算方法

元坝地区大安寨段二亚段作为页岩气勘探的新层系,存在着储层孔隙类型复杂、非均质性强、实验分析数据少、孔隙度计算方法不明确的难点。在开展页岩气储层孔隙类型分析基础上,应用6种页岩气测井解释评价技术对储层孔隙度开展计算方法研究。通过分析可知,“核磁共振测井技术”不适用,“拟合模型法”没有办法建立模型,“ANN技术”、“KNN算法”、“声波时差法”和“骨架密度法”这4种技术方法的计算孔隙度的相对误差分别是13%、13%、0.4%和3.7%,其中“声波时差法”误差最小,说明解释精度最高。因此,认为“声波时差法”是目前计算大安寨段二亚段页岩气储层孔隙度最为合适的方法。研究成果推动了元坝地区大安寨段二亚段湖相页岩气的勘探部署。