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    湖相碳酸盐岩天文旋回识别及优质储层发育特征和预测: 以西部凹陷雷家地区沙四段为例

    户昶昊 席振铢 陈昌 李阳

    户昶昊, 席振铢, 陈昌, 李阳, 2025. 湖相碳酸盐岩天文旋回识别及优质储层发育特征和预测: 以西部凹陷雷家地区沙四段为例. 地球科学, 50(12): 4715-4735. doi: 10.3799/dqkx.2025.189
    引用本文: 户昶昊, 席振铢, 陈昌, 李阳, 2025. 湖相碳酸盐岩天文旋回识别及优质储层发育特征和预测: 以西部凹陷雷家地区沙四段为例. 地球科学, 50(12): 4715-4735. doi: 10.3799/dqkx.2025.189
    Hu Changhao, Xi Zhenzhu, Chen Chang, Li Yang, 2025. Identification of Astronomical Cycles and Prediction of High-Quality Reservoir Development in Lacustrine Carbonates: A Case Study of the Fourth Member of Shahejie Formation in Leijia Area, Western Sag. Earth Science, 50(12): 4715-4735. doi: 10.3799/dqkx.2025.189
    Citation: Hu Changhao, Xi Zhenzhu, Chen Chang, Li Yang, 2025. Identification of Astronomical Cycles and Prediction of High-Quality Reservoir Development in Lacustrine Carbonates: A Case Study of the Fourth Member of Shahejie Formation in Leijia Area, Western Sag. Earth Science, 50(12): 4715-4735. doi: 10.3799/dqkx.2025.189

    湖相碳酸盐岩天文旋回识别及优质储层发育特征和预测: 以西部凹陷雷家地区沙四段为例

    doi: 10.3799/dqkx.2025.189
    基金项目: 

    辽河油田公司科技项目 2024KJZX-03

    国家科技重大专项 2024ZD1400100

    辽宁省自然科学基金计划项目 2024-BS-338

    详细信息
      作者简介:

      户昶昊(1979-),男,教授级高工,从事油气勘探开发管理工作.ORCID:0009-0000-8285-3821.E-mail:huch6@petrochina.com.cn

      通讯作者:

      李阳(1988-),男,博士后,从事石油地质和数据挖掘等相关研究工作.ORCID:0000-0001-9469-0193.E-mail:7891235@qq.com

    • 中图分类号: P624

    Identification of Astronomical Cycles and Prediction of High-Quality Reservoir Development in Lacustrine Carbonates: A Case Study of the Fourth Member of Shahejie Formation in Leijia Area, Western Sag

    • 摘要: 辽河坳陷西部凹陷雷家地区沙四段发育多套湖相碳酸盐岩,地质条件优越,具有良好资源前景,是目前该区的致密油勘探主要层系.为厘清优质储层特征和明确勘探目标,基于旋回地层学、钻测录井、地震反演以及分析测试数据识别了该区的天文旋回和分析了优质储层特征,并对优质储层“甜点”进行了预测.研究发现:(1)沙四段存在~6个长偏心率周期,~19个短偏心率周期,并弄清长偏心率旋回与该区油层组之间的关系;(2)雷家地区沙四段优质储层岩性以白云岩为主,白云石晶粒细小,多在1~3 μm分布,晶间孔隙及构造缝发育,微孔隙集中分布在0.3~0.4 μm,有效喉道长度分布在1~20 μm,孔隙体积主要分布在0.5~4.0 μm3,原油轻质组分主要赋存于裂缝和白云石晶间孔隙中,此类岩石致密且性脆,主要分布在杜三油层;(3)使用多参数融合的方法对单井进行了评价,建立储层评价标准,结合叠前地震反演资料,明确了优质储层“甜点”在层序格架内的分布规律,并进行了平面预测.研究成果进一步系统梳理了西部凹陷雷家地区沙四段地层、碳酸盐岩沉积储层特征并联合叠前地震反演有效识别该区甜点分布范围,为该区致密油勘探提供可靠的地质依据.

       

    • 图  1  渤海湾盆地辽河坳陷西部凹陷综合地质背景

      a.渤海湾盆地简图;b.辽河坳陷构造区划图;c.西部凹陷构造简图及研究区位置;d.雷15井岩性柱状图;e.西部凹陷新生界年龄分;据梁鸿德等(1992)姚益民(1994)辽河油气区编纂委员会(2022)

      Fig.  1.  Comprehensive geological background map of the western sag of the Liaohe Depression in the Bohai bay basin

      图  2  雷家地区沙四段旋回地层学分析结果

      a.雷53井岩性剖面、层序、小层以及油层组划分以及它们之间的对应关系;b.雷53井GR的偏心率滤波曲线,长偏心率滤波带宽为0.017 883±0.001 490 cycles/m,短偏心率滤波带宽为0.055 885±0.001 482 cycles/m;c.雷53井GR的2π MTM谱分析图;d.雷53井GR的eFFT分析;滑动窗口为69.9 m;e.雷93井GR的2π MTM谱分析图;f.雷88-H501导井GR的2π MTM谱分析图;g.雷37井GR的2π MTM谱分析图;h.雷97井GR的2π MTM谱分析图;i.45.4~43.0 Ma沉积时期的ETP曲线的2π MTM谱分析

      Fig.  2.  Cyclostratigraphic analysis results of the fourth member of the Shahejie Formation in the Leijia area

      图  3  不同测试方法的古沉积环境判别指标

      a.基于LA-MS-ICP测试的白云岩样品稀土元素配分模式;b.雷97井壁心和岩心碳氧同位素关系;c.不同岩性的锶同位素箱型图;d.Sr/Ba(古盐度)箱型图;e.V/(V+Ni)(古氧化还原)箱型图;f.Sr/Cu(古气候)箱型图

      Fig.  3.  Paleoenvironmental discrimination indicators derived from different analytical methods

      图  4  碳酸盐岩岩心和镜下特征

      a.纹层状泥质白云岩,白云石颗粒大小1~3 μm,晶间孔发育,雷57井,2 355.31 m,氩离子抛光扫描电镜;b.泥晶白云岩,裂缝发育,被方解石、方沸石充填,雷14井,2 766.61 m;铸体片,(+);c.泥质云岩,泥质纹层与白云石纹层互层,裂缝发育,雷37井,2 815.5 m,铸体片,(-);d.泥质云岩,压溶缝,雷97井,3 278 m,普通片,(+);e.褐灰色块状泥质白云岩,溶蚀孔洞发育,雷84井,2 649.5 m,岩心;f.泥晶云岩,泥质条带状富集,雷29-15井,2 541.68 m,普通片,(+);g.泥晶云岩,多期裂缝发育,见石膏晶模孔,雷84井,2 649.5 m,铸体片,(-);h.同(g),(+);i.含泥泥晶云岩,裂缝被方沸石充填,雷18井,2 444.4 m,铸体片,(-);j.同(j),(+);k.方沸石质云岩,方沸石与白云石均匀混合,可见长英质颗粒,裂缝发育,雷37井,2 702.5 m,铸体片,(-);l.同(k),(+)

      Fig.  4.  Core and petrographic characteristics of carbonate rocks

      图  5  储集空间类型及发育特征

      a.长英质矿物晶间孔隙,雷88-59-85井,3 484.68 m;b.黏土矿物粒间孔隙,雷21-11井,2 130.9 m;c.方解石晶间孔隙,雷37井,2 700.5 m;d.方解石晶间孔隙,雷37井,2 700.5 m;e.方沸石晶间孔隙,雷97井,3 278 m;f.黄铁矿晶间孔隙,雷15井,2 636 m;g.粒间溶蚀扩大孔,雷21-11井,2 183.82 m,铸体片,(-);h.晶模孔被方沸石充填,雷36井,2 562.6 m,铸体片,(-);i.白云石晶间溶孔,雷18井,2 466.65 m,铸体片,(-);j.有机质孔,曙150井,3 712.5 m,氩离子抛光SEM;k.方沸石晶内溶孔,雷57井,2 355.31 m,SEM;l.白云石晶内溶孔,雷88井,2 569.73 m,SEM;m.高角度构造缝和溶洞,雷29-15井,2 585.5 m,岩心;n.高角度构造缝和溶洞,雷21-11井,2 183.82 m,岩心;o.溶蚀缝和溶洞,雷57井,2 355.6 m,岩心;p.灰白色泥质云岩,溶洞,雷57井,2 365.7 m,岩心;q.灰色泥质云岩,溶洞沿裂缝走向发育,雷57井,2 363.62 m,岩心;r.层理缝,雷14井,2 771.1 m,铸体片,(-);s.多期裂缝,层理缝和高角度构造裂缝,形成裂缝网络,雷36井,2 685.47 m,铸体片,(-);t.压溶缝,雷15井,2 638.11 m,铸体片,(-);u.裂缝发育,被方解石充填,雷15井,2 610.06 m,岩心;v.裂缝被方解石(一期)和方沸石(二期)充填,雷18井,2 446.65 m,铸体片,(-);w.裂缝被方解石和方沸石充填,雷14井,2 766.61 m,铸体片,(-)

      Fig.  5.  Types and development characteristics of reservoir spaces

      图  6  白云岩样品毛细管压力曲线

      Fig.  6.  Capillary pressure curves of dolomite samples

      图  7  雷57井岩心纳米CT扫描结果

      a.孔隙空间分布图;b.样品扫描3D灰度图;c.微孔隙分布在多个区间,峰值主要分布在300 μm,600~3 000 μm区间;d. 孔隙表面积双峰分布,峰值分别为2 μm2和20 μm2;e.孔隙体积呈双峰分布,峰值分别为0.2 μm3和2 μm3;f.孔隙多为孤立微孔,2~3个微孔组成的微孔体,配位数分布在1~3;g.微孔隙集中分布在0.3~0.4 μm;h.有效喉道长度分布在1~20 μm;i.孔隙体积主要分布在0.5~4.0 μm3

      Fig.  7.  Nano-CT scanning results of core samples from Well Lei 57

      图  8  白云岩样品物性统计相关图

      a.孔隙度箱型图;b.渗透率箱型图;c.孔隙度与渗透率交汇图;d.裂缝开度与渗透率之间的关系

      Fig.  8.  Correlation and statistical diagrams of physical properties in dolomite samples

      图  9  白云岩样品原油赋存状态及激光共聚焦分析结果

      a.灰黄色白云岩,油斑,雷29-15井,2 612 m,岩心;b.灰褐色泥质云岩,富含油,雷88井,2 575.65 m,岩心;c.白云岩,原油赋存与晶间孔和溶蚀孔中,雷84井,2 647.3 m,铸体片,(-);d.方沸石质云岩,棕褐色为原油赋存于裂缝中,曙99井,3 038.38 m,铸体片,(-);e.雷57井2 355.21 m样品的荧光全貌;f.雷57井2 355.21 m样品的荧光薄片;g.雷57井2 355.21 m样品的激光共聚焦;h.雷57井2 355.21 m样品的轻重组分赋存孔隙分布;i.雷21-11井2 183.82 m样品的荧光全貌;j.雷21-11井2 183.82 m样品的荧光薄片;k.雷21-11井2 183.82 m样品的激光共聚焦;l.雷21-11井2 183.82 m样品的轻重组分赋存孔隙分布

      Fig.  9.  Crude oil occurrence states and laser confocal microscopy results in dolomite samples

      图  10  不同岩性脆性指数对比

      Fig.  10.  Comparison of brittleness index among different lithologies

      图  11  单井储层评价流程

      Fig.  11.  Single-well reservoir evaluation flowchart

      图  12  雷53井北纬65度日照量对照关系(Laskar et al., 2011; Li et al., 2025)

      Fig.  12.  Relationship between solar insolation at 65°N of Well Lei 53 (Laskar et al., 2011; Li et al., 2025)

      图  13  雷93井-雷88-H501导井-雷37井-雷97井-雷53井甜点发育规律

      a.层序格架内“甜点”分布规律,单井柱状图右边为偏心率滤波曲线;b.叠前AVO反演剖面

      Fig.  13.  Distribution pattern of reservoir sweet spots along Wells Lei 93-Lei 88-H501D-Lei 37-Lei 97-Lei 53

      图  14  西部凹陷雷家地区沙四段c7~c10层甜点评价

      Fig.  14.  Sweet spot assessment for c7-c10 layers in Es4, Leijia area, western sag

      表  1  雷93井、雷88-501导井、雷97井和雷53井MTM频谱分析结果

      Table  1.   MTM spectral analysis results for wells Lei 93, Lei 88-501dao, Lei 97, and Lei 53

      ETP 雷93 雷88-H501导 雷37 雷97 雷53
      置信度超90%周期(ka) 置信度超90%周期(ka) 峰值比 置信度超90%周期(ka) 峰值比 置信度超90%周期(ka) 峰值比 置信度超90%周期(ka) 峰值比 置信度超90%周期(ka) 峰值比
      405.00 52.91 405.00 35.18 405.00 49.44 405.00 73.98 405.00 55.92 405.00
      129.09 17.24 131.97 11.18 128.74 \ \ 22.02 120.54 17.89 129.60
      96.81 15.66 119.85 6.65 76.54 16.29 133.41 19.07 104.38 12.34 89.38
      51.52 7.56 57.86 \ \ 5.67 46.48 \ \ 6.75 48.91
      39.88 5.27 40.36 3.30 37.97 5.41 44.30 7.14 39.09 5.70 41.27
      28.65 3.41 26.10 \ \ \ \ 4.84 26.51 \ \
      23.27 \ \ 2.00 22.98 2.83 23.19 \ \ \ \
      21.99 \ \ 1.77 20.40 2.54 20.77 \ \ 3.06 22.19
      18.85 2.44 18.64 1.66 19.10 2.31 18.93 3.77 20.66 2.83 20.51
      下载: 导出CSV

      表  2  各井白云岩样品REE+Y经PAAS标准化后的数据

      Table  2.   PAAS-normalized REE+Y data of dolomite samples from each well

      井号 深度(m) REE+Y
      La Ce Pr Nd Sm Eu Gd Tb Dy Y Ho Er Tm Yb Lu
      雷88-59-85 3 504.20 0.232 0.252 0.263 0.259 0.298 0.412 0.372 0.291 0.290 0.284 0.275 0.271 0.272 0.275 0.257
      雷97 2 926.00 0.388 0.394 0.381 0.371 0.415 0.559 0.455 0.360 0.372 0.354 0.349 0.336 0.340 0.345 0.329
      雷40 2 588.55 0.272 0.289 0.264 0.263 0.322 0.418 0.326 0.307 0.322 0.337 0.313 0.311 0.305 0.290 0.270
      高34 2 710.90 0.218 0.219 0.216 0.212 0.247 0.289 0.246 0.201 0.203 0.201 0.189 0.185 0.186 0.186 0.169
      雷29-15 2 585.00 0.651 0.780 0.716 0.707 0.914 1.133 0.801 0.696 0.650 0.573 0.564 0.513 0.476 0.436 0.379
      雷14-35 2 766.61 0.161 0.178 0.172 0.175 0.222 0.295 0.243 0.209 0.233 0.259 0.230 0.237 0.247 0.249 0.233
      雷37 2 700.50 0.271 0.274 0.234 0.225 0.259 0.315 0.251 0.209 0.208 0.211 0.194 0.191 0.190 0.192 0.193
      雷93 3 081.06 0.290 0.272 0.267 0.254 0.295 0.372 0.285 0.257 0.257 0.248 0.238 0.234 0.232 0.222 0.202
      雷88 2 569.73 0.545 0.610 0.636 0.682 0.860 1.054 0.859 0.630 0.574 0.467 0.467 0.416 0.392 0.374 0.320
      雷84 2 655.50 0.647 0.644 0.609 0.584 0.747 0.928 0.708 0.647 0.624 0.612 0.587 0.574 0.583 0.580 0.520
      下载: 导出CSV

      表  3  白云岩样品压汞参数统计

      Table  3.   Statistical summary of mercury injection parameters for dolomite samples

      压汞参数 平均值(最小值~最大值)
      排驱压力(MPa) 3.037(0.008~20.064)
      孔喉平均半径(μm) 5.557(0.025~30.770)
      变异系数 1.303(0.162~5.300)
      最大汞饱和度(%) 52.840(2.40~96.06)
      最大孔喉半径(μm) 32.377(0.037~92.053)
      均质系数 0.267(0.031~0.790)
      退汞效率(%) 31.99(5.63~97.84)
      峰态 6.381(1.751~26.062)
      分选系数 7.644(0.004~35.345)
      下载: 导出CSV

      表  4  西部凹陷雷家地区沙四段储层“甜点”评价标准

      Table  4.   Evaluation criteria for reservoir "sweet spots" in Es4, Leijia area, western sag

      储层类型 地质品质 工程品质
      含油饱和度(%) TOC(%) S1(mg/g) 孔隙度(%) 优势岩性厚度(m) 脆性矿物含量(%) 杨氏模量(GPa) 地层压力系数
      Ⅰ类 ≥60 ≥3 ≥4 ≥6 ≥30 ≥60 ≥30 1.2
      Ⅱ类 40 ~60 1.5 ~3 2 ~4 3 ~6 10 ~30 40 ~60 20 ~30 1 ~1.2
      Ⅲ类 < 40 < 1.5 < 2 < 3 < 10 < 40 < 20 < 1
      下载: 导出CSV
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