Development and Hotspots of Sedimentary Response of Glutenite in the Offshore Bohai Bay Basin
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摘要: 随着全球能源需求日益增长，砂砾岩油气藏研究逐步深入，新疆准噶尔盆地玛湖大型砾岩油藏与渤海海域渤中19-6大型整装凝析气田获重大发现，使得砂砾岩体成为油气勘探新领域.当前，砂砾岩体沉积响应研究集中于陡坡背景或造山带背景，重点解析冲积扇、扇三角洲、近岸水下扇与湖底扇体系的结构样式、控制因素、沉积模式及其差异性，但机制成因方面存在多解性.渤海海域内砂砾岩体主要发育于始新世陡坡背景与中新世初期缓坡背景，其中始新世砂砾岩沿断裂陡坡带呈裙带状近源堆积，热点集中于其结构识别及期次刻画，以期准确预测地下砂砾岩体储层时空分布；而中新世初期转换界面处砂砾岩广泛分布且伴随岩浆活动，难点在于明确砂砾岩体沉积学信息、年代学信息同重大板块构造变革间响应关系，厘定大面积砂砾岩体分布的成因机制及发育模式.砂砾岩体沉积响应的研究方向将立足于完善岩相划分标准、依据，深化其与区域构造事件关联性，定量化解析沉积充填响应过程及工业化刻画其圈闭目标，系统研究对揭示渤海海域新生代盆地形成演化有重大理论意义，同时可服务大中型砂砾岩油气田的勘探需求.Abstract: With the increasing global energy consumption and deepening glutenite oil and gas reservoirs study, glutenite reservoirs have become a new field of oil and gas exploration, especially since the significant discoveries of conglomeratic reservoirs in the Mahu area, Junggar basin of Xinjiang, and integrated condensate gas field of BZ19-6 in the offshore Bohai Bay basin. At present, the research on the sedimentary response of glutenite is concentrated on the background of steep slope or orogenic belt, focusing on the analysis of the forms, structural styles, controlling factors, depositional modes and differences of alluvial fan, fan delta, nearshore subaqueous fan and sublacustrine fan systems, but there are multiple explanations for the genetic mechanism. Glutenites in the offshore Bohai Bay basin are mainly developed in Eocene steep slope background and early Miocene gentle slope background. Among them, Eocene glutenite presents a near-source accumulation along the fault steep slope belt, and the hotspots focus on its structure identification and period characterization, so as to accurately predict the spatial and temporal distribution of underground glutenite reservoirs. However, at the transition interface of the early Miocene, a set of glutenite is widely distributed and accompanied by magmatic activities. The difficulty lies in defining the response relationship between sedimentological and chronological information of glutenite and the evolution of tectonic plates, and determining the genetic mechanism and development mode of large-scale glutenite reservoirs distribution. Sedimentary response research direction of glutenite will be based on the principles and standard of lithofacies subdivision, to deepen its relationship with regional tectonic events, analyze the infilling processes quantitatively and depict its trap target of industrialization. These results would not only offer better understanding of the formation and evolution of Cenozoic Bohai Bay basin, but also facilitate the exploration of the middle and large-scale oil and gas fields with the type of glutenite in the offshore Bohai Bay basin.
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图 2 渤海海域中新世初期缓坡背景砂砾岩体平面分布
据龚再升等(2000); 张若祥等(2011); 张晓庆等(2017)
Fig. 2. Plane distribution characteristics of the glutenite systems in the early Miocene of the offshore Bohai Bay basin
图 3 基于振幅-方差体地震属性刻画断裂陡坡带砂砾体
a.原始地震振幅剖面; b.地震方差剖面; c.方差体分级三维立体图
Fig. 3. Glutenite in an rifted lacustrine basin margin characterized by amplitude-variance seismic properties
图 4 陡坡带砂砾岩体地震相控反演分析
砂砾岩复合体剖面据黄捍东等(2007)
Fig. 4. Seismic phase control inversion analysis of glutenite in an rifted lacustrine basin margin
表 1 不同成因类型砂砾岩体特征对比
Table 1. Comparison of characteristics of different genetic types of glutenite
成因类型 定义 模式图 发育位置及背景 流体流态 沉积相 岩性组合 沉积构造 生物化石 沉积序列沉积组合 构造位置 地理位置 测井相 地震相 冲积扇 一个沿山口向外伸展的锥形沉积体 常发育于断裂下降盘 陆上盆山耦合处 牵引流和重力流 扇根高幅齿化箱型与高幅齿化指状; 扇中中幅箱形或钟型; 扇端低幅平直与齿化指状 剖面上为楔形, 内部呈短波状-杂乱结构, 横剖面为丘形, 平面上呈扇形 大的角砾岩、砾岩、含砾砂岩夹薄层红色泥岩 洪积层理，交错层理，块状层理，平行层理，冲刷面及暴露构造等 基本不含或极少 主要形成内扇-中扇-外扇的下粗上细的正粒序 扇三角洲 由冲积扇提供物质并沉积在活动扇与静止水体分界面处的、全部或大部分位于水下的沉积体 可发育于陡坡带或缓坡带 陆上和浅水过渡区 牵引流和重力流 辫状河道为箱型，河道间沼泽为平直型，前缘亚相河口坝为漏斗型，支流间湾为齿型或齿化钟型 剖面上为楔形, 横剖面为丘形, 平面上呈扇形或不规则的圆形, 内部可见斜交-前积结构. 砂砾岩为主，夹泥岩、砂岩 板状，槽状交错层理，透镜状层理，波状层理 植物茎杆，浅水及间歇性暴露地表形成的化石 主要形成前扇三角洲-三角洲前缘-三角洲平原的向上变粗的反粒序 近岸水下扇 近源洪水携带大量陆源碎屑直接入湖, 并在湖盆边缘陡岸的深水环境中形成的水下扇形体 常发育于湖盆断陷鼎盛期的陡坡带 半深-深水 块体流和浊流 扇根主要为齿化箱型，扇中主要为箱形和钟型，扇端主要为锯齿型 剖面上为楔形，内部结构为杂乱-平行反射, 内扇为杂乱反射, 中扇为斜交-亚平行结构, 外扇为平行结构，其周围为“三高”的湖泊相 砾岩、砂岩、泥岩均发育，砾石含量高 块状层理，水平层理，鲍马序列，泥岩撕裂屑，包卷层理，变形层理 介形虫及双壳类 主要为内扇-中扇-外扇的向上变细的正粒序 湖底扇 湖盆中沉积物以重力流搬运方式堆积在深水区的粗碎屑扇形体，可分为滑塌型和浊积型 常发育于同生断裂下方或缓坡湖底 半深-深水 块体流和浊流 扇根主要为齿化箱型，扇中主要为复合钟型，扇端主要为齿化线型 剖面上为明显的上超充填和丘形反射, 内部呈短波-杂乱结构，其周围为平行、中振幅、高连续地震相 砂岩、泥岩为主，可见砾岩、含砾砂岩 递变层理, 斜层理, 滑塌变形构造、底模构造、鲍马序列 较大的完整鱼化石，可见深海生物觅食痕迹 单次浊流沉积为正粒序, 多次浊流形成复合体可表现为向上变粗或变细层序 参考文献：崔周旗等, 2005; Blair and McPherson, 2009; Zou et al., 2012; Cao et al., 2018; 李胜利等, 2018 
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表 2 不同构造-地貌单元的砂砾岩体发育模式
Table 2. Development patterns of glutenite with different tectonic and geomorphic units
构造 地貌 陡坡带 缓坡带 断裂样式 断裂倾角（°） 斜坡型 断阶型 板式 铲式 断阶式 坡坪式 陡(> 30) 缓(10~30) 成因类型 近岸水下扇，少量滑塌湖底扇，类型单一 近岸水下扇，少量滑塌浊积扇，低洼处发育较大规模湖底扇 冲积扇-近岸水下扇-滑塌湖底扇，类型较多 冲积扇-扇三角洲/近岸水下扇-滑塌湖底扇，类型较多 近岸水下扇-滑塌湖底扇 扇三角洲-滑塌湖底扇 浊流湖底扇 冲积扇-扇三角洲，滑塌湖底扇一般不发育，但浊流湖底扇发育 相带宽窄 窄，低位期扇体延伸较远，2~4 km 较宽，低位期扇体规模大，3~5 km 宽，砂砾岩体延伸远，5~9 km 宽，砂砾岩体沿水流方向呈链条状分布 较宽，最远可达7 km 较宽，一般为3~5 km 宽，可达8~12 km 宽，可达7~9 km 砂体分布 叠置厚度大，最厚达1 200 m 叠置厚度较大，一般不超过500 m 叠置厚度较小，一般不超过400 m 叠置厚度小，一般不超过300 m 参考文献 吴胜和等，1994；崔周旗等，2005；鄢继华等，2005；路智勇，2008；Feng et al., 2013；王星星等，2016；Cao et al., 2018
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表 3 砂砾岩体油气藏时空分布特征
Table 3. Spatial and temporal distribution characteristics of glutenite reservoirs
坳陷 凹陷 洼陷 成因类型 控制因素 沉积特征 文献来源 分布位置及层位 物源 形态及延伸距 规模面积、厚度 辽东湾 辽东 辽中 湖底扇 北部锦州20构造，东二段 胶辽隆起 厚度可达210 m 吴奎等，2012 辽西 湖底扇 西部斜坡曙二区，沙三上亚段 孤立分布 平均为200 m，最厚达400 m 孙雨等，2016 沙三中亚段 约100~400 m，最厚达500 m 吴朝容和杜春彦，2001 沙三下亚段 约50~200 m 渤中 渤中 扇三角洲 北部陡坡带CFD油田，东三段 盆内 杜晓峰等，2018 近岸水下扇 西南斜坡带25构造区，沙三段 盆内 裙带状分布 富砂区面积约为118 km2 黄凯等，2017 湖底扇 西南斜坡带21构造区，东二下段 盆内 孤立 厚可达140 m 王改卫等，2017 扇三角洲 西南斜坡带19构造脊，孔店组 盆内 裙带状分布 最大厚度可达736 m 徐长贵等，2019 秦南 扇三角洲 东南缘陡坡带，沙一-二段 裙带状分布 王冠民等，2018 沙南 扇三角洲 东北缘曹妃甸18构造，东三段 10.5~398 m 刘强虎等，2016 庙西 扇三角洲 明下和馆陶组 邹华耀等，2011 埕北 扇三角洲-湖底扇 付兆辉等，2009 莱州湾 扇三角洲 KL油田，沙四段 近180 m 韩建斌等，2018 济阳 车镇 车西 近岸水下扇 北部陡坡带沙三下段 埕宁隆起 裙带状分布 延伸距3.5~ 6.7 km，面积为41.5~57.6 km2 王星星等，2016 湖底扇 北部陡坡带沙三段 埕宁隆起 王星星等，2016 大王北 近岸水下扇 北部陡坡带沙三段 埕宁隆起 裙带状分布 朱筱敏等，2014 湖底扇 北部陡坡带沙三段 埕宁隆起 多期串珠状分布 多为3~5 m薄层, 最大单层厚为17 m 王英继和刘焕成，2013 郭局子 近岸水下扇-湖底扇 北部陡坡带沙三段 王延章等，2018 沾化 渤南 近岸水下扇 北部陡坡沙三上 北部埕东凸起 西段裙带，东段孤立 孙俊超和张立强，2018 北部陡坡带沙四上 北部埕东凸起 裙带状分布 湖底扇 洼陷中央，沙三段 孙海涛等，2013 孤北 扇三角洲 西部陡坡沙三段 盆内周缘凸起 延伸距7 km 杨剑萍等，2003 南部缓坡沙三段 延伸距2~4 km 湖底扇 洼陷中央沙三段 四扣 罗家鼻状 垦西 孤南 扇三角洲 断裂附近沙二-三段 鲁广军，2004 福林 东营 胜坨地区 近岸水下扇 北部陡坡中段，沙四上亚段 裙带状分布 单层厚度为1~ 5 m，最大68.5 m 张立强等，2015 湖底扇 北部陡坡中段，沙四上亚段 孤立分布 刘晖等，2010 盐家地区 近岸水下扇 北部陡坡，沙四上亚段 李桥等，2017 民丰 近岸水下扇 北部陡坡，沙四下亚段 王淑萍等，2014 利津 扇三角洲 滨县凸起南缓坡，沙四上亚段 张元福等，2014 牛庄 湖底扇 扇体前端，沙三中亚段 三角洲 崔杰和张伟，2015 湖底扇 东部斜坡王58地区，沙四上亚段 扇三角洲 尚冰，2011 博兴 湖底扇 西北深洼，沙三中亚段 李维岭等，2012 惠民 阳信 扇三角洲 北部陡坡，沙三-四段 无棣 厚为411.5 m 王永斌等，2016 流钟 滋镇 临南 海底扇 湖底扇 北部商三区，沙三上亚段 面积约为350 km2，厚度约为300 m 李庆等，2016 扇三角洲 江家店地区，沙四段 龚娟等，2009 里则镇 黄骅 北塘 扇三角洲 西部地区沙三段 西部物源 黄传炎等，2009 南堡 扇三角洲 北部断裂陡坡带东营组 短轴物源 刘延莉等，2008 板桥 近岸水下扇 小站地区-沧东断裂沙三段 沧县隆起 庞军刚等，2011 扇三角洲 海河断层下降盘沙三段 燕山褶皱 湖底扇 白水头以西至马棚口沙三段 歧口 近岸水下扇 南部埕北断阶带沙三、二段 埕宁隆起 孟鹏等，2005 北大港构造带 湖底扇 港中地区，沙三段 杨有星和金振奎，2012 沧东 冲积扇 东部陡坡，孔一段 张阳等，2018 南皮 湖底扇 西部斜坡底部孔二段 单层平均厚度为2.3 m，最大单层厚度为7 m 冀中 廊固 近岸水下扇 大兴断层，沙三段 大兴凸起 辫状水道细砾岩最大厚度为50 m 宋荣彩等，2007 饶阳 近岸水下扇 东北陡坡，沙三段 砂岩厚度为60~140 m 初丽兰等，2009 束鹿 湖底扇 西部斜坡，沙三段 宁晋凸起 垂向可达百米厚 郑丽婧，2016 扇三角洲 西部斜坡，沙三段 辫状河道为主体，单层厚度为1 m 临清 东濮 扇三角洲 西部斜坡北段，沙三下亚段-深陷期 内黄隆起 尹楠鑫等，2015
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