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    渤海海域沙一二段混合沉积分布特征与勘探实践

    徐伟 杜晓峰 宋章强 李正宇 李虹

    徐伟, 杜晓峰, 宋章强, 李正宇, 李虹, 2020. 渤海海域沙一二段混合沉积分布特征与勘探实践. 地球科学, 45(10): 3618-3632. doi: 10.3799/dqkx.2020.183
    引用本文: 徐伟, 杜晓峰, 宋章强, 李正宇, 李虹, 2020. 渤海海域沙一二段混合沉积分布特征与勘探实践. 地球科学, 45(10): 3618-3632. doi: 10.3799/dqkx.2020.183
    Xu Wei, Du Xiaofeng, Song Zhangqiang, Li Zhengyu, Li Hong, 2020. Distribution Characteristics and Exploration Practice of Mixed Siliciclastic-Carbonate Sediments in Bohai Sea Area. Earth Science, 45(10): 3618-3632. doi: 10.3799/dqkx.2020.183
    Citation: Xu Wei, Du Xiaofeng, Song Zhangqiang, Li Zhengyu, Li Hong, 2020. Distribution Characteristics and Exploration Practice of Mixed Siliciclastic-Carbonate Sediments in Bohai Sea Area. Earth Science, 45(10): 3618-3632. doi: 10.3799/dqkx.2020.183

    渤海海域沙一二段混合沉积分布特征与勘探实践

    doi: 10.3799/dqkx.2020.183
    基金项目: 

    国家科技重大专项 2016ZX05024-003

    详细信息
      作者简介:

      徐伟(1987-), 男, 博士, 高级工程师, 主要从事石油地质与沉积储层研究工作.ORCID:0000-0001-9544-762X.E-mail:xuwei32@cnooc.com.cn

      通讯作者:

      杜晓峰(1974-), 男, ORCID:0000-0002-2905-1886.E-mail:duxf@cnooc.com.cn

    • 中图分类号: P531

    Distribution Characteristics and Exploration Practice of Mixed Siliciclastic-Carbonate Sediments in Bohai Sea Area

    • 摘要: 渤海海域广泛发育陆源碎屑与碳酸盐矿物的混合沉积,随着近年来混积型储层的油气勘探相继获得重要发现,混合沉积分布规律亟待深入研究.基于大量基础资料,对渤海海域古近系混合沉积进行了系统性的分析,明确了其时空分布特征,完善了混合沉积相关地质认识.渤海海域古近系沙一二段(E2s1-2)主要发育以陆源碎屑为主的混积岩、以生物成因碳酸盐矿物为主的混积岩以及以化学成因碳酸盐矿物为主的混积岩三大类岩石类型.受控于干旱的气候与较高盐度的水体条件,混合沉积主要发育于沙一二段沉积时期,在空间上远离区域物源体系,主要围绕盆内局部凸起分布,低凸起、凸起倾末端、近岸隆起、远岸隆起等正向的水下古地貌单元是混合沉积发育的有利部位.根据发育位置、古地貌背景、与陆源碎屑供给的关系等古地理要素,混合沉积成因样式可分为近岸混积扇三角洲、近岸扇体侧翼混积滩坝、近岸隆起混积滩坝、远岸隆起混积滩坝4种类型及六亚类.近岸混积扇三角洲、近岸扇体侧翼混积生屑滩坝、近岸隆起混积碎屑滩坝、远岸潜山隆起混积生屑滩坝4种具体类型的混合沉积物产出规模与厚度较大,易形成粒度粗、生屑含量高、杂基含量少、白云石化作用发育、物性条件较好、产能较高的优质储层,是较为有利的勘探类型.上述地质认识有效地指导了一批混积型储层的重大勘探发现,揭示了混合沉积领域巨大的勘探潜力,对渤海海域中深层勘探具有重要的推动意义.

       

    • 图  1  渤海海域构造单元划分(a)与综合柱状图(b)

      ①辽西低凸起;②辽东凸起;③辽西南凸起;④秦南凸起;⑤石臼坨凸起;⑥沙叠田凸起;⑦埕北低凸起;⑧埕子口凸起;⑨渤东低凸起;⑩庙西北凸起;⑪庙西南凸起;⑫渤南低凸起;⑬莱北低凸起;⑭淮北凸起N;⑮淮北凸起S;⑯垦东凸起;⑰青坨子凸起;A.辽西凹陷;B.辽中凹陷;C.辽东凹陷;D.秦南凹陷;E.渤中凹陷;F.渤东凹陷;G.南堡凹陷;H.沙南凹陷;I.岐口凹陷;J.埕北凹陷;K.黄河口凹陷;L.庙西凹陷;M.莱州湾凹陷;N.莱南凹陷;O.青东凹陷

      Fig.  1.  Tectonic units (a) and synthetic column (b) of Bohai Sea area

      图  2  渤海海域沙一二段混合沉积岩石学特征

      a.含生屑砂砾岩岩心,可见生屑剥落孔,QHD29-B井,3 382.80~3 382.92 m;b.含生屑砂岩,生物碎屑主要为螺及其碎片,QHD36-A井,3 772.15 m;c.含生屑砂岩,生物碎屑主要为螺及其碎片,LD25-A井,3 287.50 m;d.砂质生屑云岩岩心,断面见大量生物颗粒,QHD36-A井,3 775.50 m;e.含砂生屑云岩岩心,生屑颗粒均匀,JZ20-A井,2 221.50 m;f.含砂生屑云岩,生屑以螺化石碎片为主,大量生物溶蚀孔隙,QHD36-A井,3 766.43 m;g.含砂鲕粒云岩,BZ36-W井,2 389.50 m;h.含粉砂泥晶白云岩,BZ36-W井,2 388.60 m

      Fig.  2.  Petrologic characteristics of E2s1-2 mixed sedimentation in Bohai Sea area

      图  3  渤海海域沙一二段混积岩沉积特征

      Fig.  3.  Sedimentary characteristics of E2s1-2 mixed sedimentation in Bohai Sea area

      图  4  渤海海域古近系混合沉积发育比例

      Fig.  4.  Development ratio of Paleogene mixed sedimentation in Bohai Sea area

      图  5  渤海海域沙一二段碳氧同位素特征

      Fig.  5.  Isotope of carbon and oxygen of E2s1-2 in Bohai Sea area

      图  6  渤海海域混合沉积钻井分布与基底地貌叠合

      Fig.  6.  Superimposed map of basement topography and distribution of mixed sedimentation in Bohai Sea area

      图  7  渤海海域古近系混合沉积成因模式

      Fig.  7.  Genetic pattern of Paleogene mixed sedimentation in Bohai Sea area

      图  8  渤海海域古近系混积型优质储层微观特征

      a.含生屑砂砾岩,原生孔隙发育,QHD36-A井,3 771.68 m;b.含生屑中-粗砂岩,碎屑颗粒以石英为主,并普遍发育泥晶白云石包壳,原生粒间孔隙发育,LD25-A井,3 287.50 m;c.含砂生屑云岩,生物碎片与溶蚀孔隙大量发育,QHD36-A井,3 766.83 m;d.含砂生屑云岩,见完整螺化石壳体及体腔溶蚀孔隙,CFD2-A井,3 426.30 m;e.含生屑砂砾岩,阴极发光,碎屑颗粒普遍发育橘红色白云石包壳,QHD29-B井,3 376.48 m;f.白云质砂岩,扫描电镜,碎屑颗粒周边发育白云石包壳,LD25-A井,3 302.00 m

      Fig.  8.  Microscopic characteristics of Palaeogene mixed reservoir in Bohai Sea area

      图  9  秦皇岛29地区近岸混积扇三角洲沉积储层特征

      a.秦皇岛29近岸混积扇发育模式;b.QHD29-B井综合柱状图

      Fig.  9.  Sedimentary and reservoir characteristics of near-shore mixed fan delta in Qinhuangdao 29 area

      图  10  LD25-A井近岸隆起混积碎屑滩坝沉积储层特征

      a.LD25-A井沙一二段取心段综合柱状图;b.LD25-A井3 287.50 m砂岩粒度样本分布图;c.LD25-A井砂岩储层特征,含生屑,原生孔隙发育,3 290.00 m;d.LD25-A井砂岩储层特征,含生屑,原生孔隙发育,3 299.00 m

      Fig.  10.  Sedimentary and reservoir characteristics of mixed siliciclastic beach bar on near-shore uplift of LD25-A

      图  11  锦州20地区远岸潜山隆起混积生屑滩坝沉积储层特征

      a.锦州20地区远岸混积生屑滩坝沉积模式;b.JZ20-A井取心段沉积特征;c.含砂生屑灰岩,JZ20-A井,可见生物溶蚀孔,2 222.20 m;d.锦州20地区储层孔隙度特征

      Fig.  11.  Sedimentary and reservoir characteristics of mixed biological beach bar on offshore buried hill of JZ20 area

      表  1  渤海海域秦皇岛29构造区微量元素及古环境特征

      Table  1.   Microelement and paleoenvironment features of QHD29 area in Bohai Sea area

      井名 层位 深度(m) Sr (μg/g) Cu (μg/g) Ba (μg/g) Sr/Cu 古环境 Sr/Ba 古水体
      QHD29-B 东三段 2 942.50 209 25.30 5 000 8.260 870 温润气候 0.041 800 淡水
      3 047.50 219 25.80 5 000 8.488 372 0.043 800
      3 147.50 211 32.50 5 000 6.492 308 0.042 200
      沙一二段 3 317.50 504 16.80 5 000 30.000 000 干热气候 0.100 800 淡水
      3 332.50 580 18.20 5 000 31.868 130 0.116 000
      3 342.14 676 5.10 701 132.549 000 干热气候 0.964 337 半咸水
      3 344.00 429 41.50 557 10.337 350 0.770 197
      3 367.45 362 3.87 485 93.540 050 0.746 392
      3 371.96 431 5.90 348 73.050 850 1.238 506 咸水
      3 376.50 443 5.26 434 84.220 530 1.020 737
      3 378.92 418 4.72 334 88.559 320 1.251 497
      3 380.06 614 6.37 676 96.389 320 0.908 284 半咸水
      3 384.75 446 15.30 617 29.150 330 0.722 853
      3 427.50 1119 9.78 5 000 114.417 200 0.223 800 淡水
      3 592.50 571 98.60 5 000 5.791 075 温润气候 0.114 200
      3 682.50 427 32.70 5 000 13.058 100 干热气候 0.085 400
      下载: 导出CSV

      表  2  渤海古近系混合沉积成因背景及岩相特征

      Table  2.   Geological setting and lithofacies features of Paleogene mixed sedimentation in Bohai Sea area

      成因类型 亚类 古地貌背景 与陆源碎屑关系 岩相特征 典型构造
      近岸混积扇三角洲 混积扇三角洲 盆内局部凸起近源陡坡带 与近岸扇三角洲伴生 主要发育以陆源碎屑为主的混积岩相,厚度大 秦皇岛29
      近岸扇体侧翼混积滩坝 混积生屑滩坝 盆内局部凸起近源陡坡带、斜坡带 碎屑沉积体侧翼,陆源碎屑干扰作用弱 主要发育以生屑等碳酸盐颗粒为主混积岩相,厚度较大 秦皇岛36、绥中36
      近岸隆起混积滩坝 混积粒屑滩坝 近岸的古地貌高地 废弃三角洲之上 主要发育以生屑、鲕粒为主的混积岩相,厚度较薄 渤中36、渤中27
      混积碎屑滩坝 三角洲远端或侧翼,碎屑干扰作用较弱 以三角洲为物质基础,在波浪作用下发育厚层砂质滩坝,含少量生屑 旅大25
      远岸隆起混积滩坝 混积生屑滩坝 远岸的水下潜山基底隆起 远离陆源碎屑干扰 潜山基底上主要发育含少量陆源碎屑的生屑碳酸盐岩混积岩相,垂向厚度大 锦州20、渤中13、曹妃甸2
      混积泥晶滩 远岸的水下泥质基底隆起 泥质基底上主要发育泥晶碳酸盐为主的混积岩相 秦皇岛30
      下载: 导出CSV

      表  3  不同类型混合沉积储层综合评价

      Table  3.   Comprehensive evaluation of different types of mixed reservoirs

      成因类型 产出厚度(m) 平面规模(km2) 粒屑含量 埋深(m) 主要成岩特征 物性(平均孔隙度) 产能 实例
      近岸混积扇三角洲 200~240 10~30 15%左右 3 400 弱压实、弱溶蚀 17.8% 秦皇岛29
      近岸扇体侧翼混积生屑滩坝 20~40 10左右 60%左右 3 700 强溶蚀、弱胶结 27.6% 秦皇岛36
      近岸隆起混积粒屑滩坝 2~7 15左右 60%左右 2 400 中溶蚀、中胶结 15.7% 一般 渤中36
      近岸隆起混积碎屑滩坝 5~30 10~15 10%~15% 3 300 中压实、弱胶结 25.4% 旅大25
      远岸潜山隆起混积生屑滩坝 20~60 20~40 60%~70% 2 200 强溶蚀、弱胶结 23.2% 较高 锦州20
      远岸泥质隆起混积泥晶滩坝 2~10 5~8 5%左右 3 000 强压实、强胶结 6.5% 秦皇岛30
      下载: 导出CSV
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