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    饶阳凹陷沙一下亚段优质烃源岩地球化学特征及成藏贡献

    杨帆 王权 郝芳 郭柳汐 邹华耀

    杨帆, 王权, 郝芳, 郭柳汐, 邹华耀, 2021. 饶阳凹陷沙一下亚段优质烃源岩地球化学特征及成藏贡献. 地球科学, 46(1): 172-185. doi: 10.3799/dqkx.2019.249
    引用本文: 杨帆, 王权, 郝芳, 郭柳汐, 邹华耀, 2021. 饶阳凹陷沙一下亚段优质烃源岩地球化学特征及成藏贡献. 地球科学, 46(1): 172-185. doi: 10.3799/dqkx.2019.249
    Yang Fan, Wang Quan, Hao Fang, Guo Liuxi, Zou Huayao, 2021. Biomarker Characteristics of Lower Sub-Member of the First Member of the Shahejie Formation and Its Accumulation Contribution in Raoyang Depression, Jizhong Sub-Basin. Earth Science, 46(1): 172-185. doi: 10.3799/dqkx.2019.249
    Citation: Yang Fan, Wang Quan, Hao Fang, Guo Liuxi, Zou Huayao, 2021. Biomarker Characteristics of Lower Sub-Member of the First Member of the Shahejie Formation and Its Accumulation Contribution in Raoyang Depression, Jizhong Sub-Basin. Earth Science, 46(1): 172-185. doi: 10.3799/dqkx.2019.249

    饶阳凹陷沙一下亚段优质烃源岩地球化学特征及成藏贡献

    doi: 10.3799/dqkx.2019.249
    基金项目: 

    国家重大基金项目 41690134

    国家自然科学基金项目 U1663210

    中国石油华北油田科技项目"饶阳-霸县凹陷环境-生物协同演化与优质烃源岩发育分布及其成藏贡献研究" HBYT-YJY-2014-JS

    详细信息
      作者简介:

      杨帆(1993-), 男, 博士研究生, 主要从事油气地球化学, 油气成藏等研究.ORCID:0000-0002-9838-9450.E-mail:chinaofjz@163.com

    • 中图分类号: P632

    Biomarker Characteristics of Lower Sub-Member of the First Member of the Shahejie Formation and Its Accumulation Contribution in Raoyang Depression, Jizhong Sub-Basin

    • 摘要: 为了研究饶阳凹陷沙一下亚段优质源岩的地球化学特征及其成藏贡献.基于有机碳、热解、生烃模拟实验评价源岩生烃潜力;基于源岩GC-MS实验和生烃潜力评价结果,描述源岩分子地球化学及有机相特征,利用多元数理统计方法,建立油-岩关系并定量计算原油中各源岩贡献率,总结了沙一下亚段成藏贡献规律.研究表明:沙一下亚段源岩的生烃潜力在凹陷内发育的3套源岩中最大,并且ω(伽马蜡烷)/ω(C30藿烷)、ω(甾烷)/ω(藿烷)等生物标志物参数与其他两套源岩有明显区别.原油样品可以划分为沙一下亚段来源,沙一下和沙三段混源和沙三上和下段混源3种成因类型.成藏贡献计算结果显示沙一下亚段源岩总贡献率达到58%,对东营组、馆陶和明化镇组原油贡献达到77%,对沙河街组原油贡献达到66%.饶阳凹陷沙一下亚段源岩是一套非常优质的烃源岩,成藏贡献大,应得到更多关注.沙一下亚段源岩高贡献区分布受到地质条件、成藏模式和源岩有机相控制,古近系和新近系储层原油主要来源于沙一下亚段源岩.

       

    • 图  1  饶阳凹陷主要洼槽、油田分布

      Fig.  1.  Primary sags and the location of oil fields of Raoyang depression

      图  2  饶阳凹陷沙一下亚段Tmax(℃)和HI(hydrogen index)(mg HC/g TOC)的关系

      Fig.  2.  Relationship of Tmax (℃) vs. HI (mg HC/g TOC) for the E2s3L in the Raoyang depression

      图  3  饶阳凹陷沙一下亚段TOC(%)和S1+S2 (mg HC/g Rock)的关系图

      Fig.  3.  Relationship of TOC(%) vs. S1+S2 (mg HC/g Rock) for the E2s3L in the Raoyang depression

      图  4  饶阳凹陷与渤海湾盆地源岩样品热模拟产物与Easy%Ro关系

      Fig.  4.  Relationship between products of pyrolysis and Easy%Ro of source rock samples in the Raoyang depression and Bohai Bay basin

      图  5  饶阳凹陷典型源岩的萜烷(m/z=191)和甾烷(m/z=217)质量色谱图

      Fig.  5.  Representative mass chromatograms of terpane (m/z=191) and sterane (m/z=217) series of saturate fractions for the three sets of source rocks intervals in the Raoyang depression

      图  6  饶阳凹陷烃源岩生物标志物参数组合特征

      Fig.  6.  Characteristics of biomarker parameter assemblages of source rocks in the Raoyang depression

      图  7  饶阳凹陷原油成因类型划分

      Fig.  7.  Division of crude oil genetic tapes in the Raoyang depression

      图  8  饶阳凹陷原油ALS-C分析结果

      B代表八里庄油田, D代表大王庄油田, G代表高阳油田, H代表河间油田, LB代表留北油田, LC代表留楚油田, LX代表留西油田, N代表南马庄油田, R代表任丘油田, S代表肃宁油田, X代表西柳油田;层位1代表了东营组、馆陶和明化镇组储层; 层位2代表沙河街组储层,层位3代表前第三系储层主要包括潜山储层包括奥陶系、寒武系、蓟县系雾迷山组

      Fig.  8.  Analytic results of crude oil in the Raoyang depression by using ALS-C

      图  9  饶阳凹陷原油ALS-C计算端元生物标志物比值与源岩比值关系

      Fig.  9.  Relationship between caculated by ALS-C biomarker ratio of crude oils and ratio of source rocks in the Raoyang depression

      图  10  饶阳凹陷源岩成藏贡献分布特征

      Fig.  10.  Distribution charcteristics of accumulation contribution of source rocks in the Raoyang depression

      表  1  饶阳凹陷烃源岩生物标志物参数

      Table  1.   Biomarker parameters of source rocks in the Raoyang depression

      井名 层位 深度(m) C19/C23TT C24TET/C26TT S/H Pr/Ph G/H C27DiaST/C27ST C35/C34SH ETR
      西63 E2s1L 3 175.5 0.24 1.63 2.65 0.35 0.29 0.13 0.46 0.59
      西63 E2s1L 3 207.5 0.15 1.41 2.22 0.29 0.29 0.07 0.54 0.66
      西63 E2s1L 3 214.0 0.17 1.44 2.41 0.31 0.31 0.07 0.54 0.60
      西63 E2s1L 3 227.0 0.17 1.60 2.73 0.20 0.44 0.06 0.57 0.63
      西63 E2s1L 3 242.0 0.19 1.51 2.99 0.26 0.37 0.06 0.48 0.60
      西63 E2s1L 3 278.0 0.13 1.32 2.16 0.29 0.40 0.09 0.50 0.58
      西63 E2s1L 3 262.5 0.12 1.22 2.90 0.27 0.60 0.09 0.58 0.71
      西63 E2s1L 3 288.0 0.16 1.01 3.02 0.28 0.47 0.07 0.56 0.65
      西63 E2s1L 3 307.5 0.14 1.20 2.79 0.26 0.43 0.08 0.54 0.64
      西63 E2s1L 3 323.0 0.17 1.18 2.70 0.32 0.58 0.09 0.57 0.79
      阳探1 E2s1L 4 036.0 0.34 1.45 2.16 0.58 0.31 0.17 0.48 0.65
      阳探1 E2s1L 4 129.0 0.21 0.65 2.03 0.54 0.43 0.13 0.46 0.74
      阳探1 E2s1L 4 190.5 0.19 0.59 2.99 0.51 0.36 0.25 0.63 0.67
      楚深1 E2s1L 3 849.7 0.11 0.39 1.64 0.49 0.35 0.18 0.50 0.66
      西37 E2s1L 3 165.7 0.11 1.09 2.51 0.27 0.84 0.08 0.56 0.63
      西9 E2s1L 2 721.2 0.21 1.63 5.51 0.20 0.35 0.05 0.89 0.61
      西柳11 E2s1L 3 424.4 0.16 1.24 3.83 0.19 0.62 0.06 0.49 0.78
      西63 E2s3U 3 615.0 0.22 0.81 1.47 0.64 0.27 0.26 0.46 0.45
      西63 E2s3U 3 710.0 0.19 0.83 1.29 0.49 0.20 0.31 0.54 0.51
      西63 E2s3U 3 723.5 0.23 0.99 1.17 0.45 0.22 0.29 0.46 0.47
      西63 E2s3U 3 744.0 0.16 0.91 1.51 0.42 0.35 0.35 0.48 0.48
      阳探1 E2s3U 4 410.0 0.24 0.53 0.92 0.56 0.24 0.30 0.53 0.55
      阳探1 E2s3U 4 553.5 0.23 0.60 1.04 0.64 0.21 0.23 0.53 0.57
      阳探1 E2s3U 4 603.5 0.25 0.46 1.09 0.49 0.19 0.28 0.53 0.60
      阳探1 E2s3U 4 675.5 0.26 0.68 1.06 0.57 0.20 0.29 0.55 0.55
      阳探1 E2s3U 4 734.0 0.16 0.63 1.05 0.59 0.18 0.26 0.55 0.51
      宁302 E2s3U 4 131.1 0.38 0.88 1.12 0.67 0.11 0.29 0.40 0.36
      宁35 E2s3U 3 748.5 0.20 0.47 0.99 0.64 0.19 0.29 0.50 0.44
      马99 E2s3L 4 012.0 0.38 1.46 0.80 0.41 0.09 0.14 0.39 0.37
      马99 E2s3L 4 042.0 0.31 1.23 0.88 0.30 0.14 0.08 0.42 0.41
      下载: 导出CSV

      表  2  饶阳凹陷沙一下亚段有机相划分(Chen et al., 2018

      Table  2.   The classification of organic facies of Es1L in the Raoyang depression(Chen et al., 2018)

      有机相类型 A B C
      沉积环境 深湖-半深湖 半深湖-浅湖 滨岸-浅湖
      氧化还原条件 强还原 还原-弱还原 弱还原-弱氧化
      有机质来源 水生生物 混合较少陆源植物的水生生物 以陆源植物为主
      TOC(%) > 2 1.5~4.0 0.7~2.6
      S1+S2 (mg/g rock) > 15 5~20 2~10
      HI (mg/g TOC) > 450 300~500 130~350
      干酪根类型 Ⅰ-Ⅱ Ⅱ-Ⅲ
      烃类产物 主要油,少量气 油和气
      下载: 导出CSV

      表  3  饶阳凹陷原油生物标志物参数

      Table  3.   Biomarker parameters of crude oils in the Raoyang depression

      编号 井号 层位 油田 R1 R2 R3 R4 R5 R6 R7 R8
      1 高30-211斜井 E2s1 高阳 0.14 0.86 3.93 0.22 0.47 0.08 0.52 0.71
      2 西柳1 E2s1 西柳 0.13 1.05 4.18 0.22 0.42 0.07 0.48 0.65
      3 西柳10-25斜井 E2s2 西柳 0.16 0.95 4.18 0.22 0.45 0.07 0.56 0.74
      4 高9-1井 E2s2 高阳 0.14 1.03 4.86 0.18 0.50 0.06 0.54 0.72
      5 路32-5井 Nm 大王庄 0.16 0.84 2.59 0.25 0.39 0.09 0.48 0.68
      6 路36-30斜1井 Ng 留西 0.16 0.83 2.85 0.25 0.39 0.10 0.48 0.66
      7 路27-18井 Ng 留北 0.15 0.81 2.69 0.27 0.40 0.10 0.47 0.69
      8 高30-226斜井 E3d 高阳 0.12 0.73 2.61 0.26 0.38 0.09 0.51 0.74
      9 留414井 E3d 大王庄 0.14 0.84 2.96 0.24 0.42 0.11 0.54 0.67
      10 间9井 E3d 八里庄 0.17 0.85 2.57 0.25 0.40 0.09 0.46 0.66
      11 宁49-5斜井 E3d 西柳 0.13 0.70 2.31 0.28 0.37 0.09 0.50 0.72
      12 任121井 E2s3 任丘 0.29 1.17 1.79 0.29 0.31 0.11 0.51 0.60
      13 任111井 E2s1 任丘 0.22 1.30 1.82 0.30 0.35 0.13 0.52 0.61
      14 马95-28井 E3d 南马庄 0.23 1.23 2.08 0.28 0.33 0.18 0.46 0.62
      15 宁81井 E2s1 八里庄 0.26 0.91 1.49 0.53 0.38 0.16 0.47 0.49
      16 西6-9斜井 E2s1 南马庄 0.30 1.39 1.59 0.30 0.29 0.19 0.50 0.63
      17 马425井 E2s2 南马庄 0.24 1.32 1.98 0.32 0.33 0.12 0.49 0.63
      18 西36-18井 E3d 南马庄 0.31 1.45 1.45 0.32 0.27 0.10 0.48 0.61
      19 西20井 Jxw 南马庄 0.35 1.32 1.44 0.33 0.28 0.15 0.46 0.65
      20 任4井 Jxw 任丘 0.20 1.14 1.82 0.30 0.35 0.08 0.50 0.53
      21 西31斜井 E2s2 八里庄 0.30 1.24 2.00 0.28 0.36 0.13 0.49 0.59
      22 路47-12井 E2s1 留西 0.15 0.88 1.91 0.42 0.28 0.15 0.44 0.67
      23 留416-7井 E2s3 留西 0.16 0.88 2.02 0.41 0.33 0.17 0.49 0.67
      24 留70-303斜井 E2s1 大王庄 0.18 0.74 1.42 0.40 0.23 0.14 0.47 0.53
      25 留70-137井 E2s3 大王庄 0.19 0.57 1.60 0.42 0.43 0.20 0.53 0.53
      26 楚107井 E3d 留楚 0.19 0.72 1.72 0.38 0.38 0.15 0.48 0.53
      27 间213斜井 E3d 河间 0.25 0.86 1.78 0.50 0.32 0.11 0.45 0.49
      28 宁93斜井 E2s1 肃宁 0.16 0.64 1.38 0.35 0.23 0.11 0.44 0.48
      29 强65斜井 E2s1 武强 0.28 0.95 1.35 0.40 0.31 0.25 0.61 0.47
      30 强2-34井 E2s2 武强 0.33 1.13 1.41 0.42 0.34 0.22 0.54 0.49
      31 强49-9井 Ng 武强 0.29 1.01 0.92 0.41 0.22 0.23 0.51 0.48
      32 马15井 Pt1 八里庄 0.31 1.25 1.02 0.40 0.15 0.19 0.46 0.43
      33 马851-3井 Jxw 河间 0.25 0.74 1.28 0.42 0.20 0.17 0.48 0.49
      34 留67斜1井 Jxw 留北 0.23 0.66 1.13 0.48 0.17 0.20 0.51 0.44
      35 任802 任丘 0.28 1.31 0.90 0.43 0.17 0.20 0.45 0.40
      36 宁古8-3斜1井 Jxw 肃宁 0.45 1.27 0.72 0.38 0.07 0.15 0.43 0.36
      37 任85井 O 任丘 0.35 1.61 0.63 0.35 0.12 0.12 0.44 0.38
      注:O代表奥陶系; ∈代表寒武系; Jxw代表中元古蓟县系; Pt1代表古元古界;R1代表C19/C23TT; R2代表C24TET/C26TT; R3代表S/H; R4代表Pr/Ph; R5代表G/H; R6代表C27DiaST/C27ST; R7代表C35/C34 SH; R8代表ETR
      下载: 导出CSV
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