Graded and Quantitative Technology and Application of Coal-Bearing Reservoir Based on Seismic Reflection Characteristics

Taiyuan formation is the main exploration strata in Ordos Basin, and coals are widely developed. Due to the interference of strong reflection of coals, we cannot completely identify the effective reservoir information of coal-bearing reservoir on seismic data. Previous researchers have studied the reservoir by stripping or weakening the strong reflection, but it is difficult to determine the effectiveness of the remaining reflection seismic data. In this paper, through the establishment of 2D forward model of coal-bearing strata, the corresponding geophysical characteristics of different reflection types of coal-bearing strata are analyzed, and then the favorable sedimentary facies zones for reservoir development are predicted. On this basis, combined with seismic properties, the coal-bearing reservoir is quantitatively characterized by seismic inversion. The above research shows that the Taiyuan formation in LS block of Ordos Basin is affected by coals and forms three or two peaks in different locations. The reservoir plane sedimentary facies zone is effectively characterized by seismic reflection structure. Based on the characteristics of sedimentary facies belt and petrophysical analysis, the reservoir is semi quantitatively characterized by attribute analysis and waveform indication, and quantitatively characterized by pre stack geostatistical inversion. Based on the forward analysis of coal measure strata, this technology characterizes the reservoir facies belt through seismic reflection characteristics, and describes coal measure reservoirs step by step. It effectively guides the exploration of LS block in Ordos Basin, and has achieved good practical application effect.

Experimental study of the dynamic mechanical responses and failure characteristics of coal under true triaxial confinements

Investigations on the dynamic mechanical properties and failure mechanisms of coal under in-situ stress is essential for the prevention of dynamic disasters in deep coal mines.Thus,a modified true triaxial Hopkinson bar was employed to explore the dynamic mechanical behaviors of coal at different confining pressures(0–20 MPa)and strain rates(40–220 s^(-1)).The results show that the dynamic peak stress is positively correlated with lateral static pre-stressσy andσz,but negatively correlated with axial static prestressσx.At approximate strain rates,increasing the lateral static pre-stress facilitates increasing the dynamic peak stress,but the minimum lateral static pre-stress is the primary factor limiting a significant increase in dynamic peak stress of coal.Furthermore,the dynamic differential stress is linearly related to the logarithm of strain rate,and the peak strain varies linearly with strain rate.However,there is no significant correlation between confining pressure and peak strain.Moreover,X-ray CT images and photographic fracture observations of coal samples show the failure patterns under uniaxial and triaxial conditions are splitting failure and shear failure,respectively.The device provides a viable approach for fully comprehending the dynamic mechanical behaviors of rock-like material in complex stress conditions.

Coalbed Methane-bearing Characteristics and Reservoir Physical Properties of Principal Target Areas in North China

The coalbed methane (CBM) resources in North China amounts up to 60% of total resources in China. North China is the most important CBM accumulation area in China. The coal beds of the Upper Paleozoic Taiyuan and Shanxi formations have a stable distribution. The coal reservoir of target areas such as Jincheng, Yanquan-Shouyang, Hancheng, Liulin, etc. have good CBM-bearing characteristics, high permeability and appropriate reservoir pressure, and these areas are the preferred target areas of CBM developing in China. The coal reservoirs of Wupu, Sanjiaobei, Lu'an, Xinmi, Anyang-Hebi, Jiaozuo, Xinggong and Huainan also have as good CBM-bearing characteristics, but the physical properties of coal reservoirs vary observably. So, further work should be taken to search for districts with high pressure, high permeability and good CBM-bearing characteristics. Crustal stresses have severe influence on the permeability of coal reservoirs in North China. From west to east, the crustal stress gradient increases, while the coal reservoirs permeability decreases.

Geological characteristics and co-exploration and co-production methods of Upper Permian Longtan coal measure gas in Yangmeishu Syncline, Western Guizhou Province, China

Coal measure gas(also known as coal-bearing unconventional gas)is the key field and development direction of unconventional natural gas in recent years.The exploration and evaluation of coal measure gas(coalbed methane,coal shale gas and coal measure tight sandstone gas)from single coalbed methane has greatly expanded the field and space of resource evaluation,which is of positive significance for realizing the comprehensive utilization of coal resources,maximizing the benefits and promoting the innovation of oil and gas geological theory and technological advances in exploration and development.For the first time,in Yangmeishu Syncline of Western Guizhou Province,the public welfare coalbed methane geological survey project of China Geological Survey has been carried out a systematic geological survey of coal measure gas for the Upper Permian Longtan Formation,identified the geological conditions of coal measure gas and found high quality resources.The total geological resource quantity of coalbed methane and coal shale gas is 51.423×109 m3 and the geological resource abundance is up to 566×106 m3/km2.In this area,the coal measures are characterized by many layers of minable coal seams,large total thickness,thin to the medium thickness of the single layer,good gas-bearing property of coal seams and coal measure mudstone and sandstone,good reservoir physical property and high-pressure coefficient.According to the principle of combination of high quality and similarity of key parameters of the coal reservoir,the most favorable intervals are No.5-2,No.7 and No.13-2 coal seam in Well YMC1.And the pilot tests are carried out on coal seams and roof silty mudstone,such as staged perforation,increasing hydraulic fracturing scale and"three gas"production.The high and stable industrial gas flow with a daily gas output of more than 4000 m3 has been obtained,which has realized the breakthrough in the geological survey of coal measure gas in Southwest China.Based on the above investigation results,the geological characteristics of coal measure gas in the multi-thin-coal-seam-developed area and the coexploration and co-production methods,such as the optimization method of favorable intervals,the highefficiency fracturing and reservoir reconstruction method of coal measures,and the"three gas"drainage and production system,are systematically summarized in this paper.It will provide a reference for efficient exploration and development of coal measure gas in similar geological conditions in China.

Pore Characteristics of the Fine-Grained Tight Reservoirs in the Yabulai Basin, Northwestern China

This work investigated the pore structure characteristics and reservoir features of the finegrained tight reservoirs in the lower member of the Xinhe Formation(J2x1) in the Xiaohu subsag,Yabulai Basin based on core samples through various techniques. Interbedded silt/fine sandstones and mudstones are developed in the study area. Scanning electron microscopy(SEM) images were used to delineate different types of pores, including primary intergranular pores, secondary intergranular and intragranular pores, organic pores and fractures. The pore types were distinguished by pore size, pore area, location and formation process. The pore radii of the fine-grained rocks range from 1 nm to 1.55μm, mainly concentrated between 5 and 300 nm by low pressure N2adsorption and MICP analyses. The pore structure parameters of pore throat size and pore throat sorting coefficient are both positively correlated with porosity, while pore throat sorting coefficient has a negative correlation with permeability. The pore structures of the studied samples are much related to the mineral type and content and grain size, followed by TOC content. In these rocks with relatively low TOC and low maturity, the rigid minerals protect pores with pressure shadow from collapse, and dissolution-related pores contribute a lot to inorganic porosity. In contrast, these rocks with abundant TOC contain a large number of organic pores. The permeability of the fine-grained tight reservoir is mainly dominated by larger pore throats, while a large number of small pores(mostly <0.1 μm) contribute considerably to porosity. These results have deepened our understanding of the interbedded fine-grained tight reservoirs and can be applicable to fine-grained reservoirs in a similar setting.

Permeability variation characteristics of coal after injecting carbon dioxide into a coal seam

A theoretical basis for the optimization of carbon dioxide injection parameters and the development of the drainage system can be provided by identifying the permeability change characteristic of coal and rock after injection of carbon dioxide into the coal seam. Sihe, Yuwu, and Changcun mines were used as research sites. Scanning electron microscopy and permeability instruments were used to measure coal properties such as permeability and surface structure of the coal samples at different p H values of carbon dioxide solution and over different timescales. The results show that the reaction between minerals in coal and carbonate solution exhibit positive and negative aspects of permeability-the dissolution reaction between carbonate minerals in coal and acid solution improves the conductivity of coal whilst, on the other hand, the clay minerals in the coal(mainly including montmorillonite, illite and kaolinite) exhibit expansion as a result of ion exchange with the H+in acid solution, which has a negative effect on the permeability of the coal. The permeability of coal samples increased at first and then decreased with immersion time, and when the soaking time is 2–3 months the permeability of the coal reached a maximum. In general, for coals with permeabilities less than 0.2 m D or greater than 2 m D, the effect on the permeability is low; when the permeability of the coal is in the range 0.2–2 m D, the effect on the permeability is highest. Research into permeability change characteristics can provide a theoretical basis for carbon dioxide injection under different reservoir permeability conditions and subsequent drainage.

A Comprehensive Appraisal on the Characteristics of Coal-Bed Methane Reservoir in Turpan-Hami Basin

The rich coal-bed methane resources in the Turpan-Hami Basin are mainly located in the Shisanjianfang,Hami,Shanshan,Sha'erhu,Kekeya,Kerjian,Aidinghu inclines and the Dananhu coal-bed methane reservoirs. The big-ger coal-bed reservoirs are sitting at a depth of less than 1500 m. The coalbed methane generation,storage and confin-ing conditions of the Turpan-Hami basin can be indicated by eight key parameters. They are coal-bed thickness,coal rank,missing period,permeability,Langmuir volume,rock covering ability,structural confinement and hydrodynamic sealing environment. These parameters constitute a comprehensive appraisal index system of the coal-bed methane res-ervoir characteristics of the Turpan-Hami basin. In these parameters,the missing period of coal-bed methane is indi-cated by a stratum missing intensity factor. It reflects the relative exposure period of coal series. The results of a fuzzy comprehensive judgment showed that the Shisanjianfang coal-bed methane reservoir has the best prospects for exploita-tion and the Sha'erhu,Shanshan,Hami coal-bed methane reservoirs are next in line.

Characteristics of Coalbed Methane Resources of China

The paper deals with the coalbed methane gas-bearing characteristics such as the gas content, theoretical gas saturation, gas concentration and abundance, as well as coal reservoir characteristics such as the adsorption, desorption and permeability of China's coal reservoirs. The paper also introduces the resources of coalbed methane with a gas content ≥ 4 m3/t and their distribution in China.

Comparative experimental study on porosity, mechanical and CO_(2) adsorption characteristics of coal and shale

To compare the pore structure, mechanical and CO_(2) adsorption properties of coal and shale, a series of experiments were carried out using nuclear magnetic resonance (NMR), uniaxial compression, Brazilian splitting, and high-pressure CO_(2) adsorption. The results show that the total porosity of coal is 7.51 times that of shale, and shale is dominated by adsorption pores, while adsorption pores and seepage pores in coal are equally important. Moreover, it is found that the micropores in shale are more advantageous, while meso-macropore in coal are more significant. The adsorption pore surface of coal is rougher than that of shale, and the seepage pore structure of shale is more complex. The uniaxial compressive strength, elastic modulus and absorption energy of shale are 2.01 times, 2.85 times, and 1.27 times that of coal, respectively, indicating that shale has higher compressive capacity and resistance to elastic deformation than coal. The average tensile strength, Brazilian splitting modulus, absorbed energy and brittleness index of shale are 7.92 times, 6.68 times, 10.78 times, and 4.37 times that of coal, respectively, indicating that shale has higher tensile strength and brittleness, but lower ductility, compared with coal. The performed analyses show that under the same conditions, the CO_(2) adsorption capacity of coal is greater than that of shale. The present article can provide a theoretical basis to implement CO_(2)-enhanced coalbed methane (CBM)/shale gas extraction.

不同应力路径下层理煤体力学特性试验研究

为探究不同应力路径下层理煤体力学特性和破坏特征,利用MTS816岩石力学试验系统对0°、30°、45°、60°和90°层理倾角煤样开展了常规三轴加载、增轴压卸围压和恒轴压卸围压应力路径下的力学试验,分析了应力路径和层理倾角对煤样强度、变形及破坏特征的影响规律。研究结果表明:(1)常规三轴加载条件下煤样在达到峰值强度前,应力-应变曲线呈近线性关系,达到峰值强度后,应力-应变曲线迅速跌落;增轴压卸围压条件下,随着卸荷比的增加,轴向应变增量比呈线性增加趋势,而环向应变增量比和体积应变增量比呈低速增长-急剧增长-平稳增长的三阶段变化特征;恒轴压卸围压条件下,轴向应变增量比、环向应变增量比和体积应变增量比均呈低速增长-急剧增长的两阶段变化特征。(2)随着层理倾角的增加,不同应力路径下煤样峰值强度和轴向峰值应变均呈先减小后增大的V型变化趋势,在0°时达到最大值,在60°时达到最小值。(3)随着卸荷比的增大,煤样变形模量先平缓后迅速劣化,泊松比先缓慢增加后呈指数形式增加,临界卸荷比随层理倾角的增大先增加后减小;当层理倾角相同时,增轴压卸围压条件下的临界卸荷比低于恒轴压卸围压。(4)常规三轴加载条件下煤样发生脆性剪切破坏,增轴压卸围压和恒轴压卸围压条件下煤样呈张拉-剪切混合破坏模式,当层理倾角为60°时,煤样主剪切破裂面角度与层理倾角几乎一致。

川中侏罗系自流井组大安寨段页岩油储层特征及其勘探启示

为进一步指导四川盆地侏罗系自流井组大安寨段页岩油的勘探与开发,亟需理清页岩油的有利赋存岩相。通过岩心观察、薄片鉴定、高压压汞、核磁共振、岩石热解等实验,分析大安寨段页岩层系不同岩相的储集空间类型、孔隙结构特征及含油性。结果表明,大安寨段主要发育块状(泥质)介壳灰岩、层状泥质介壳灰岩、层状介壳页岩、纹层状含介壳页岩、块状含介壳黏土质页岩和页理状含粉砂黏土质页岩6类岩相;页岩物性远优于介壳灰岩,且随着灰质含量的增加孔径逐渐增大,但总孔体积和总连通体积逐渐减小;大安寨段页岩层系平均游离油(S1)值为1.31 mg/g,含油性中等,页理状含粉砂黏土质页岩与纹层状含介壳页岩S1值较高,分别为2.37 mg/g与1.82 mg/g。页理状含粉砂黏土质页岩和纹层状含介壳页岩的储集性较好、含油性较高,两者构成的岩相组合可作为大安寨段页岩油的重点勘探对象。

致密砂岩气藏与页岩气藏展布模式

在阐述美国和中国致密砂岩气和页岩气资源潜力和年产量的基础上,系统梳理致密砂岩气藏与页岩气藏展布的研究沿革,分析页岩气藏、致密砂岩气藏展布特征及致密砂岩气成因类型。研究表明:(1)美国致密砂岩气在天然气总产量中占比由2008年的35%降至2023年的8%左右;美国页岩气2023年产量为8310×10^(8)m^(3),在天然气总产量中占比由2000—2008年的5%~17%升至2023年的70%以上。(2)中国致密砂岩气占天然气总产量比例由2010年的16%升至2023年的28%以上;2012年中国开始生产页岩气,2023年产量达250×10^(8)m^(3),约占天然气全国总产量的11%。(3)页岩气藏展布模式为连续型,根据页岩气藏是否有断层切割及断距与气层厚度的关系,连续型页岩气藏可分为连续式和断续式两种。(4)与以往大部分学者认为致密砂岩气藏展布模式为连续型的认识不同,致密砂岩气藏展布模式不是连续型;根据圈闭类型,致密砂岩气藏可分为岩性型、背斜型和向斜型3种。(5)中国3大克拉通盆地和埃及Obavied次盆的致密砂岩气为煤成气,美国阿巴拉契亚盆地和阿曼迦巴盐盆地的致密砂岩气为油型气。

海孜煤矿深部勘查区中组煤层气储层物性特征分析

【目的】煤层气储层的物性特征是进行煤层气开发研究的关键因子。【方法】重点对海孜煤矿深部勘探区域中组煤储层的物性参数进行调查,以对井田内中组煤储层物性特征进行研究。【结果】研究表明,煤层的物性特征适宜开采,其中有机显微组分占优,无机显微组分次之。该煤层含气量多,虽然煤层渗透率相对较小,但符合煤层气开采条件。煤层开采时的吸附作用一般,但有利于煤层气储集和缩短煤层气的开发周期。【结论】研究结果可为该研究区煤层气抽采提供可靠的技术参考。

层状复合夹煤岩石组合体试样强度试验与破坏特征研究

针对巷道复合夹煤组合结构顶板易冒落问题,以某矿取芯和钻孔窥视探测获得的巷道层状复合夹煤顶板结构组合类型为实验背景,对砂质泥岩、中砂岩以及煤厚度为20、30、40 mm不同结构组合类型的复合试件进行了单轴压缩试验,研究了复合夹煤岩石组合体的力学特性与破坏特征。试验结果表明:复合夹煤岩石组合体的抗压强度均小于单一岩石,中砂岩夹煤厚度为30mm时抗压强度达到单一中砂岩抗压强度的85.95%,抗压强度随着煤厚变薄而下降;砂质泥岩夹煤厚度为20 mm时仅为单一砂质泥岩抗压强度的32.5%,随着夹煤厚度增加抗压强度也增大,夹煤厚度超过30mm后抗压强度增大不明显。复合夹煤岩石组合体整体呈X状共轭斜面剪切破坏、单斜面剪切破坏、部分拉伸破坏,随着复合夹煤岩石组合类型不同呈现不同的破坏特征等。

Physical characteristics of high-rank coal reservoirs in different coal-body structures and the mechanism of coalbed methane production

The physical characteristics of coal reservoirs are important for evaluating the potential for gas desorption,diffusion,and seepage during coalbed methane(CBM)production,and influence the performance of CBM wells.Based on data from mercury injection experiments,low-temperature liquid nitrogen adsorption,isothermal adsorption,initial velocity tests of methane diffusion,and gas natural desorption data from a CBM field,herein the physical characteristics of reservoirs of high-rank coals with different coal-body structures are described,including porosity,adsorption/desorption,diffusion,and seepage.Geometric models are constructed for these reservoirs.The modes of diffusion are discussed and a comprehensive diffusion-seepage model is constructed.The following conclusions were obtained.First,the pore distribution of tectonically deformed coal is different from that of normal coal.Compared to normal coal,all types of pore,including micropores(<10 nm),transitional pores(10-100run),mesopores(100-1000 nm),and macropores(>1000 nm),are more abundant in tectonically deformed coal,especially mesopores and macropores.The increase in pore abundance is greater with increasing tectonic deformation of coal;in addition,the pore connectivity is altered.These are the key factors causing differences in other reservoir physical characteristics,such as adsorption/desorption and diffusion in coals with different coal-body structures.Second,normal and cataclastic coals mainly contain micropores.The lack of macropores and its bad connectivity limit gas desorption and diffusion during the early stage of CBM production.However,the good connectivity of micropores is favorable for gas desorption and diffusion in later gas production stage.Thus,because of the slow decline in the rate of gas desorption,long-term gas production can easily be obtained from these reservoirs.Third,under natural conditions the adsorption/desorption properties of granulated and mylonitized coal are good,and the diffusion ability is also enhanced.However,for in situ reservoir conditions,the high dependence of reservoir permeability on stress results in a weak seepage of gas;thus,desorption and diffusion is limited.Fourth,during gas production,the pore range in which transitional diffusion takes place always increases,but that for Fick diffusion decreases.This is a reason for the reduction in diffusion capacity,in which micropores and transitional pores are the primary factors limiting gas diffusion.Finally,the proposed comprehensive model of CBM production under in situ reservoir conditions elucidates the key factors limiting gas production,which is helpful for selection of reservoir stimulation methods.

重质油组成与结构对油煤浆流变性能的影响

新疆低阶煤和重质油资源丰富,具有广阔的煤油共液化工业前景,但重质油自身流动性差,极大地限制了煤油共液化的发展。为认识重质油组成结构对油煤浆流变性能的影响,选取5种性质差异明显的重质油和2种工业循环溶剂油,探究其与上湾煤形成的油煤浆流变性能变化规律,在此基础上通过预加氢调控减压渣油的组成结构,分析重质油组成、结构与流变性能,获得重质油组成结构对油煤浆流变性能的影响规律。结果表明,重质油本身是牛顿流体,加入煤粉后转变为假塑性流体,呈现剪切稀化特征;重质油中胶质和沥青质组分含量越高,形成油煤浆的黏度越高,体系内部的触变结构越丰富,非牛顿流体特征越明显。减压渣油稠油预加氢后,形成油煤浆的黏度显著降低,其中,380℃下预加氢2 h后制成的油煤浆黏度在135℃时降至451 mPa·s,同时油煤浆的触变特性也明显减弱。预加氢促使减压渣油中的长链断裂为短链烃,胶质和沥青质组分转化为饱和分与芳香分,从而抑制胶团的生成,降低油煤浆黏度。其中,380℃下预加氢2 h后胶质含量较未处理减少约21%,重均分子量降至1594 Da,芳香环β位的H含量增加约20%。

准噶尔盆地南缘西段齐古组深层储层特征及物性控制因素

准噶尔盆地南缘西段齐古组深层碎屑岩储层油气勘探潜力巨大,但目前针对其储层特征及物性控制因素尚缺乏系统研究,制约了后期油气勘探进程。本文综合利用铸体薄片、扫描电镜、物性、压汞及包裹体等资料,并结合区域埋藏史及古地温等相关成果,对齐古组储层岩石学特征、物性特征、成岩作用特征及物性控制因素进行系统研究。结果表明,齐古组储层具有低成分成熟度、高塑性岩屑含量及中等结构成熟度的岩石学特征。尽管储层主体埋深大于3500 m,但储集空间仍以粒间孔为主,平均孔隙度为10.29%,平均渗透率为34.12×10^(-3)μm^(2),总体上属低孔低渗储层,但仍发育部分中-高孔渗储层。储层成岩作用主要有压实作用、胶结作用及溶蚀作用,成岩强度相对较弱,主体处于早成岩B期—中成岩A期,并表现为压实强度中等、胶结物含量较低且晚期发育酸性溶蚀的特征。富石英与长石、贫岩屑以及分选好等特征有利于储层物性的保存,而储层物性损失以压实减孔最为显著,但储层内部绿泥石包壳及中成岩期的酸性溶蚀作用可有效改善储层物性。此外,齐古组地层早期长期浅埋、后期短期快速深埋、地层超压及较低的古地温梯度等因素延缓了储层成岩进程,进而降低成岩作用强度,导致齐古组优质储层得以有效保存。

东营凹陷古近系页岩组构及典型岩相储集特征

基于岩石薄片、扫描电镜、显微荧光和阴极发光等图像学分析方法,结合核磁共振、氮气吸附等测试技术,对东营凹陷古近系碳酸盐矿物类页岩相和混合类页岩相2种典型岩相进行研究。根据矿物组分和产状将页岩划分为碳酸盐纹层和泥质纹层2类结构单元,通过分析两者的矿物类型及相关孔隙发育特征,揭示了2种典型岩相储集特征,并根据埋藏过程中地质要素的相对变化,讨论了页岩层系储集空间发育条件。研究结果表明:东营凹陷古近系页岩矿物组分多样,以多组分碳酸盐矿物普遍发育、多来源长英质碎屑颗粒局部集中以及黏土矿物和有机质等流变性组分塑性充填为特征。骨架颗粒限定了有机组分的分布边界,有机组分内部又包含部分自生矿物,孔隙充填物受原油沥青质和蜡质含量高、地表凝固点高等因素的影响,有机组分与无机矿物间显示出多重嵌合特征。页岩组构与复杂的演化过程共同决定了孔隙类型和发育机制的多样性,碳酸盐矿物类页岩相发育纳米级晶内孔隙和微米级晶间孔隙及溶蚀孔隙,以孔隙大且连通好为特征,孔隙度相对偏低;混合类页岩相发育纳米-微米级黏土矿物片间孔隙,孔隙小且连通差,孔隙度相对偏高。层间缝发育区具有良好的储集性,储集空间由富含基质孔隙的多尺度孔缝网络构成,在整体富有机质的背景下,古近系富碳酸盐页岩具有基质普遍含油和纹层界面富集的特征。

沁水盆地榆社—武乡区块二叠系煤系页岩储层地质建模及“甜点”预测

沁水盆地煤系页岩气资源丰富,但勘探开发处于初期阶段。基于钻井、测井和地震解释资料,结合有机地球化学与储层物性实验测试数据,通过三维地质建模技术,建立了沁水盆地榆社—武乡区块二叠系山西组底部—太原组上部煤系页岩地质模型,并预测了煤系页岩气“甜点”区。研究结果表明:(1)沁水盆地榆社—武乡区块石炭系—二叠系煤系地层模型反映了煤系页岩储层的发育主要受控于构造活动,呈“东浅西深、整体连续”的分布格局。(2)基于序贯指示法建立沉积相模型,指示研究区在太原期—山西期由海陆过渡相转变为近海陆相沉积环境,为稳定优质页岩储层的形成提供了有利的沉积环境。(3)通过相控属性建模实现了储层参数空间分布模拟和精细表征,泥地比、孔隙度、含气量、总有机碳含量和镜质体反射率的平均值分别为0.57,10.02%,1.21 m^(3)/t,2.18%,2.45%,揭示了研究区煤系页岩较好的储集能力、含气性、有机质丰度和资源潜力,脆性指数模型指示出页岩压裂后的有利区带。(4)在精细三维地质建模的基础上,将三维网格单元赋值积分,计算研究区二叠系煤系页岩气地质资源量为1 344.98×10^(8)m^(3),运用层次分析法和模糊评价法预测页岩气“甜点”区,Ⅰ类“甜点”区为地质与工程双重甜点,分布于研究区东北部、中部和西北部局部区域。