石油与天然气地质 ›› 2024, Vol. 45 ›› Issue (4): 1121-1141.doi: 10.11743/ogg20240416
刘成龙1(), 王艳忠1(), 杨怀宇2, 操应长1, 王淑萍3, 郭超凡1, 郭豪1, 陈兆祥1, 宋林坤1, 黄歆媛1
收稿日期:
2024-01-21
修回日期:
2024-07-16
出版日期:
2024-09-05
发布日期:
2024-09-05
通讯作者:
王艳忠
E-mail:liuchenglongupc@163.com;wyzh@upc.edu.cn
第一作者简介:
刘成龙(2000—),男,博士研究生,沉积学与层序地层学。E-mail: liuchenglongupc@163.com。
基金项目:
Chenglong LIU1(), Yanzhong WANG1(), Huaiyu YANG2, Yingchang CAO1, Shuping WANG3, Chaofan GUO1, Hao GUO1, Zhaoxiang CHEN1, Linkun SONG1, Xinyuan HUANG1
Received:
2024-01-21
Revised:
2024-07-16
Online:
2024-09-05
Published:
2024-09-05
Contact:
Yanzhong WANG
E-mail:liuchenglongupc@163.com;wyzh@upc.edu.cn
摘要:
为研究断陷盆地斜坡带低位体系域岩性圈闭发育,以渤海湾盆地济阳坳陷东营凹陷南坡东段沙河街组四段上亚段(沙四上亚段)低位体系域为研究对象,利用岩心、测录井资料,开展了高精度层序划分对比、层序动态演化和沉积微相平面精细刻画研究。研究表明:沙四上亚段低位体系域划分为3个准层序组、9个准层序,发育6种准层序、4种准层序组以及5种体系域地层叠加样式,经历9次准层序级别相对湖平面升降,在相对湖平面下降期物源供给充足,平面上由盆缘进积为主型向盆内进积型过渡分布。主要发育三角洲-滩坝沉积体系,包括扇三角洲、三角洲和滩坝3种沉积相以及7种沉积微相类型。东营凹陷南坡东段沙四上亚段低位体系域内部以坝主体和滩脊微相尖灭砂体为储集体,以准层序和准层序组底部湖侵泥岩为局部盖层、水进体系域泥岩为区域盖层,形成岩性圈闭。
中图分类号:
图2
东营凹陷南坡东段沙四上亚段低位体系域内部准层序组、准层序界面特征及划分a. 面2井层序地层划分; b. 沉积过程、低位体系域与基准面升降关系(①—④: Vail等[67-69]定义的低位体系域; ①—②: 强制水退阶段,沉积间断; ②—③: 强制水退阶段, 基准面下降速率减慢; ③—④: 正常水退阶段, 基准面上升且速率不断加快; MFS: 最大水进面; BSFR: 强制水退底面, 基准面最高; CC: 相对应整合面, 基准面最低; MRS: 最大水退面); c1.低位体系域界面,莱115井,埋深2 885.88 ~ 2 887.65 m,岩心照片; c2. 莱115井, 埋深2 886.18 m, 灰褐色油泥岩, 岩心照片; c3. 莱115井, 埋深2 887.43 m, 浪成砂纹交错层理细砂岩, 岩心照片; c4.准层序界面,王580井,埋深3 174.00 ~ 3 175.80 m,岩心照片; c5. 王580井, 埋深3 173.00 m, 黑色水平层理泥岩, 岩心照片; c6. 王580井,埋深3 175.45 m, 浪成砂纹交错层理粉砂岩, 岩心照片; c7.准层序组界面,王149井,埋深1 678.00 ~ 1 679.90 m,岩心照片; c8. 王149井, 埋深1 679.05 m, 灰色水平层理泥岩, 岩心照片; c9. 王149井, 埋深1 679.40 m, 浪成砂纹交错层理粉砂岩-细砂岩, 岩心照片"
图4
东营凹陷南坡东段沙四上亚段纯下次亚段准层序、准层序组层序动态演化过程a1. 准层序进积1型, 面2井, 准层序9; a2. 准层序进积2型, 王123井、准层序1(左), 王斜119井、准层序5(右); a3. 准层序进积3型, 王151井, 准层序8; a4. 准层序进积4型, 王121井, 准层序5; a5. 准层序对称型, 王956井, 准层序3; a6. 准层序退积为主型, 面13井, 准层序9; b1. 准层序组进积1型, 王斜119, 准层序组2; b2. 准层序组进积2型, 王121井, 准层序组2; b3. 准层序组对称型, 面13井, 准层序组3; b4. 准层序组进积为主型, 王956, 准层序组1"
图7
东营凹陷南坡东段沙四上亚段低位体系域(扇)三角洲相特征a. 扇三角洲相水下分流河道微相单井沉积学特征,王955-斜1井;b. 三角洲相水下分流河道微相单井沉积学特征,王斜128井;c.三角洲相河口坝微相单井沉积学特征,王斜98井; d. 王955-斜1井, 埋深1 317.00 m, 灰绿色含砾杂砂岩, 岩心照片; e. 王斜128井, 埋深2 699.40 m, 槽状交错层理粗砂岩, 岩心照片; f. 王斜128井, 埋深2 700.60 m, 平行层理粗砂岩, 岩心照片; g. 角4井, 埋深1 828.71 m, 灰绿色泥砾岩, 岩心照片; h. 角4井, 埋深1 840.16 m, 泥砾、冲刷面, 岩心照片; i. 王斜98井, 埋深2 150.50 m, 浪成砂纹层理复合粒序细砂岩, 岩心照片; j. 角4井, 埋深1 847.43 m,流水砂纹层理粉砂岩, 岩心照片; k. 王斜128井, 埋深2 699.30 m, 二段式粒度概率累积曲线"
图8
东营凹陷南坡东段沙四上亚段低位体系域滩坝相特征a. 滩坝相坝主体微相单井沉积学特征,王125井;b. 滩坝相坝侧缘微相单井沉积学特征,王123井;c.滩坝相滩脊、滩席微相单井沉积学特征,王123井; d. 王125井, 埋深2 776.15 m, 浪成砂纹层理细砂岩, 岩心照片; e. 王斜98井, 埋深2 153.40 m, 浪成砂纹层理细砂岩, 岩心照片; f. 王152-5井, 埋深1 537.90 m, 浪成砂纹层理粉砂岩, 岩心照片; g 王127井, 埋深3 122.14 m, 浪成砂纹层理细砂岩, 岩心照片; h. 莱115井, 埋深2 895.75 m, 上攀层理粉砂岩, 岩心照片; i. 莱115井, 埋深2 903.30 m, 波状层理粉砂岩, 岩心照片; j. 王123井, 埋深2 300.20 m, 透镜状层理粉砂岩, 岩心照片;k. 王125井, 埋深2 784.20 m, 三段式粒度概率累积曲线"
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