准噶尔盆地白家海凸起西山窑组一段低渗储层地质成因及优质储层分布规律
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摘要
白家海凸起位于准噶尔盆地腹部，为一SW向倾伏的鼻状凸起，是新疆石油分公司彩南油田作业区重要的勘探开发区块。该凸起构造高部位（彩9—彩10井区）西山窑组一段发育大型构造岩性油藏，储层总体表现为中孔、低渗（孔隙度平均值为14.6%，渗透率平均值为2.81×10-3μm2）的特点。目前该区块已进入高含水阶段的开发中后期；但因储层低渗的地质成因与优质储层分布的认识不清，导致了开发中难于理清油水分布规律，在压裂开发的增产措施中出现高含水，注采矛盾突出，制约了该油田高效开发。
论文以层序地层学与储层沉积学理论指导，从岩心描述与测井资料的分析入手，结合地震与生产动态资料，系统开展了工区层序地层格架、构造特征、古地理背景、沉积相展布以及储层成岩作用等方面的研究；并结合典型井生产历史，深入分析了储层低渗的主要地质成因，预测了优质储层的分布，为该油区后续开发调整与滚动勘探开发的评价提供了可靠的地质依据。论文主要创新点与结论如下：
（1）通过井震结合再现古地貌的研究，表明西山窑沉积时研究区为一SW向的宽缓型单斜，受北部与北东向沉积物源影响，区内发育了东（彩10井区）、西（彩9井区）两大沉积体系。西部为2个朵叶状三角洲，多以厚层砂体叠加连片分布为特点，单井平均累积厚度为23.1m左右，测井曲线常呈箱状，为多期水下分流河道和河口坝叠置而成；而东部为4个鸟足状三角洲，中－薄层砂体发育，砂体常呈孤立分布特征，单井平均累积厚度为10.3m左右，测井曲线多为钟型，主要由水下分流河道形成。
（2）研究区西一段低渗储层的地质成因主要有三个方面，一为粒度细（均值3Φ）、塑性火山岩岩屑含量高（平均含量为17%），致使孔隙喉道的压实率明显大于孔隙部位；二为高岭石胶结物堵塞喉道明显；三是早成岩阶段，上覆煤层所产生的酸性水溶液加速了硅酸盐矿物和方解石矿物的溶解；由于这三个方面的综合影响，导致砂岩储层喉道迅速变细（喉道半径范围为0~5μm），从而极大降低了储层的渗透率，形成了中孔低渗的特点。
（3）优质储层主要受沉积时的水动力条件控制，尤其是地形平缓部分水动力较强的各类水道（主河道、水下分支河道），其塑性颗粒含量少，物性好，为I类储层；而地形略有转折的部位多形成河口坝，其沉积速度和塑性颗粒含量均大于河道，致使其物性也较河道要差可定为II类优质储层。
（4）优质储层平面分布受砂体规模、沉积微相类型、有效储层厚度控制，将三种控制因素叠合分析，预测了其分布区域；西部优质储层平面展布方向与水下分流河道主流向一致，形态呈条带状；而东部呈孤立状。
Baijiahai high is located in the centre of Junggar Basin. It is a nose-like high trendingsouthwest and one of the important exploratory and developmental blocks of Cainan oilfieldof PetroChina Xinjiang Oilfield Company. The large-scale structural and lithologic trapsystem was developed in1stmember of Xishanyao Formation in structural high part of theuplift (Cai9-Cai10well area). It is generally characterized by low-middle porosity and lowpermeability (the average porosity is14.6%and the average permeability is2.81×10-3μm2).The block has been in high water cut stage during the middle and later Period of OilfieldDevelopment. However, the knowledge of geological genesis of low permeability reservoirand distribution of high quality reservoir are not clear which makes it difficult to resolve theproblem of the oil-water distribution law in development. Furthermore, high water cut stageoccurs during fracturing development period presenting serious injection-productionproblem which restricts the efficient development of the oilfield.
Under the guidance of sequence stratigraphy and reservoir sedimentology and throughthe analysis of core description, logging, seismic and production performance data, Isystematically study stratigraphic framework, structural feature, paleogeo graphy, faciesdistribution and reservoir diagenesis. By integrating with typical well production history,main geological genesis of low-permeability reservoir and distribution law of high-qualityreservoirs are deeply analysed which provide reliable basis for subsequent developmentadjustment, progressive evaluation of exploration and development of the oil region. Themain innovation and conclusion of the thesis are as follows:
(1) Through the study of the palaeogeomorphology by analyzing well data and seismicdata, the results indicate the research area was a wide-gentle NW-trend homocline duringthe period of Xishanyao Formation. Two large-scale depositional systems were developed inthe East(Cai10-well area) and West(Cai9-well area) under the influence of sedimentsupply from the north and northeast source area.Two lobate–type deltas with thick layer ofsand bodies which stacked and distributed contiguously were formed in the west area.Owing to multiphase stacked braided subaqueous distributary channels, single well dataindicates the average cumulative thickness of sand was23.1m and is characterized bybox-shaped in common. In contrast, four birdfoot-type deltas were formed in the east. Thecharacteristics of sand bodies are moderate-thin layer of sand and isolated distribution.Single well data indicated average cumulative thickness was10.3m, and well logging curveshape is bell.
(2) Three major aspects about geological origin of low permeability reservoirs in thestudy were obtained. Firstly, because of the fine particle size (mean3Φ) and high plastic volcanic debris content (average content of17%), the compaction rate of pore throats issignificantly greater than that of pore. Secondly, throats were plugged by kaolinite cementslargely. Thirdly, the acidic water solution generated from overlying coal seam acceleratesthe dissolution of silicate minerals. Due to the combined effects of these three aspects, thethroat of sandstone reservoirs rapidly becomes thinner (throat radius range from0to5μm),reducing the permeability of the reservoir greatly, and the reservoir is characterized bymoderate porosity and low permeability. Furthermore, the high reservoir irreducible watersaturation results in water flooded seriously during the early fracturing development stage,whereas oil production remained relatively stable in the later stage.
(3) High quality reservoir is mainly controlled by the sedimentary hydrodynamiccondition; The strong hydrodynamic channels at gentle slope (main channel, subaqueousdistributary channel) are characterized by less plastic particles and good physical property.These channels belong to reservoir typeⅠ. Whereas the mouth bar are always formed atsites where gradients of slope are changing. The sedimentation rate, particle size and thecontent of plastic particles are larger than the channel sandstone which are classified asreservoir type II. The characteristics of reservoir of this type are poor physical property.
(4) The high-quality reservoir are influenced and controlled by the scale of sand body,distribution of sedimentary facies and effective thickness of sandstone. According to theanalysis of these three controlling factors, the distribution of reservoir was predicted. Thedirection of reservoir distribution in the west is consistent with the direction of the mainsubaqueous distributary channel. The shape of the reservoir on flat surface in the west islike string whereas the shape of reservoir in the east is isolated.
论文以层序地层学与储层沉积学理论指导，从岩心描述与测井资料的分析入手，结合地震与生产动态资料，系统开展了工区层序地层格架、构造特征、古地理背景、沉积相展布以及储层成岩作用等方面的研究；并结合典型井生产历史，深入分析了储层低渗的主要地质成因，预测了优质储层的分布，为该油区后续开发调整与滚动勘探开发的评价提供了可靠的地质依据。论文主要创新点与结论如下：
（1）通过井震结合再现古地貌的研究，表明西山窑沉积时研究区为一SW向的宽缓型单斜，受北部与北东向沉积物源影响，区内发育了东（彩10井区）、西（彩9井区）两大沉积体系。西部为2个朵叶状三角洲，多以厚层砂体叠加连片分布为特点，单井平均累积厚度为23.1m左右，测井曲线常呈箱状，为多期水下分流河道和河口坝叠置而成；而东部为4个鸟足状三角洲，中－薄层砂体发育，砂体常呈孤立分布特征，单井平均累积厚度为10.3m左右，测井曲线多为钟型，主要由水下分流河道形成。
（2）研究区西一段低渗储层的地质成因主要有三个方面，一为粒度细（均值3Φ）、塑性火山岩岩屑含量高（平均含量为17%），致使孔隙喉道的压实率明显大于孔隙部位；二为高岭石胶结物堵塞喉道明显；三是早成岩阶段，上覆煤层所产生的酸性水溶液加速了硅酸盐矿物和方解石矿物的溶解；由于这三个方面的综合影响，导致砂岩储层喉道迅速变细（喉道半径范围为0~5μm），从而极大降低了储层的渗透率，形成了中孔低渗的特点。
（3）优质储层主要受沉积时的水动力条件控制，尤其是地形平缓部分水动力较强的各类水道（主河道、水下分支河道），其塑性颗粒含量少，物性好，为I类储层；而地形略有转折的部位多形成河口坝，其沉积速度和塑性颗粒含量均大于河道，致使其物性也较河道要差可定为II类优质储层。
（4）优质储层平面分布受砂体规模、沉积微相类型、有效储层厚度控制，将三种控制因素叠合分析，预测了其分布区域；西部优质储层平面展布方向与水下分流河道主流向一致，形态呈条带状；而东部呈孤立状。
Baijiahai high is located in the centre of Junggar Basin. It is a nose-like high trendingsouthwest and one of the important exploratory and developmental blocks of Cainan oilfieldof PetroChina Xinjiang Oilfield Company. The large-scale structural and lithologic trapsystem was developed in1stmember of Xishanyao Formation in structural high part of theuplift (Cai9-Cai10well area). It is generally characterized by low-middle porosity and lowpermeability (the average porosity is14.6%and the average permeability is2.81×10-3μm2).The block has been in high water cut stage during the middle and later Period of OilfieldDevelopment. However, the knowledge of geological genesis of low permeability reservoirand distribution of high quality reservoir are not clear which makes it difficult to resolve theproblem of the oil-water distribution law in development. Furthermore, high water cut stageoccurs during fracturing development period presenting serious injection-productionproblem which restricts the efficient development of the oilfield.
Under the guidance of sequence stratigraphy and reservoir sedimentology and throughthe analysis of core description, logging, seismic and production performance data, Isystematically study stratigraphic framework, structural feature, paleogeo graphy, faciesdistribution and reservoir diagenesis. By integrating with typical well production history,main geological genesis of low-permeability reservoir and distribution law of high-qualityreservoirs are deeply analysed which provide reliable basis for subsequent developmentadjustment, progressive evaluation of exploration and development of the oil region. Themain innovation and conclusion of the thesis are as follows:
(1) Through the study of the palaeogeomorphology by analyzing well data and seismicdata, the results indicate the research area was a wide-gentle NW-trend homocline duringthe period of Xishanyao Formation. Two large-scale depositional systems were developed inthe East(Cai10-well area) and West(Cai9-well area) under the influence of sedimentsupply from the north and northeast source area.Two lobate–type deltas with thick layer ofsand bodies which stacked and distributed contiguously were formed in the west area.Owing to multiphase stacked braided subaqueous distributary channels, single well dataindicates the average cumulative thickness of sand was23.1m and is characterized bybox-shaped in common. In contrast, four birdfoot-type deltas were formed in the east. Thecharacteristics of sand bodies are moderate-thin layer of sand and isolated distribution.Single well data indicated average cumulative thickness was10.3m, and well logging curveshape is bell.
(2) Three major aspects about geological origin of low permeability reservoirs in thestudy were obtained. Firstly, because of the fine particle size (mean3Φ) and high plastic volcanic debris content (average content of17%), the compaction rate of pore throats issignificantly greater than that of pore. Secondly, throats were plugged by kaolinite cementslargely. Thirdly, the acidic water solution generated from overlying coal seam acceleratesthe dissolution of silicate minerals. Due to the combined effects of these three aspects, thethroat of sandstone reservoirs rapidly becomes thinner (throat radius range from0to5μm),reducing the permeability of the reservoir greatly, and the reservoir is characterized bymoderate porosity and low permeability. Furthermore, the high reservoir irreducible watersaturation results in water flooded seriously during the early fracturing development stage,whereas oil production remained relatively stable in the later stage.
(3) High quality reservoir is mainly controlled by the sedimentary hydrodynamiccondition; The strong hydrodynamic channels at gentle slope (main channel, subaqueousdistributary channel) are characterized by less plastic particles and good physical property.These channels belong to reservoir typeⅠ. Whereas the mouth bar are always formed atsites where gradients of slope are changing. The sedimentation rate, particle size and thecontent of plastic particles are larger than the channel sandstone which are classified asreservoir type II. The characteristics of reservoir of this type are poor physical property.
(4) The high-quality reservoir are influenced and controlled by the scale of sand body,distribution of sedimentary facies and effective thickness of sandstone. According to theanalysis of these three controlling factors, the distribution of reservoir was predicted. Thedirection of reservoir distribution in the west is consistent with the direction of the mainsubaqueous distributary channel. The shape of the reservoir on flat surface in the west islike string whereas the shape of reservoir in the east is isolated.
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