济阳坳陷义和庄凸起东部燕山期构造负反转及层序地层样式响应

宋广增; 徐蒙; 李磊; 孙迪; 刘辉

doi:10.3799/dqkx.2018.519

济阳坳陷义和庄凸起东部燕山期构造负反转及层序地层样式响应

doi: 10.3799/dqkx.2018.519

宋广增^1,2,,
徐蒙³,
李磊⁴,
孙迪⁵,
刘辉⁶

1.
济南大学资源与环境学院, 山东济南 250022
2.
中国地质大学构造与油气资源教育部重点实验室, 湖北武汉 430074
3.
山东省第一地质矿产勘查院, 山东济南 250014
4.
中海石油(中国)有限公司湛江分公司, 广东湛江 524057
5.
中国石化胜利油田石油开发中心有限公司, 山东东营 257000
6.
山东省物化探勘查院, 山东济南 250013

基金项目:

项目编号

详细信息

作者简介:
宋广增(1987-), 男, 讲师, 博士, 从事盆地分析研究及相关教学工作, 主要从事构造-层序地层研究

中图分类号: P539.2
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出版历程
- 收稿日期: 2018-10-13
- 刊出日期: 2019-02-15

Yanshanian Tectonic Inversion and the Response of Sequence Stratigraphic Patterns in Eastern Yihezhuang Salient, Jiyang Depression, Bohai Bay Basin

Song Guangzeng^{1,2
,},
Xu Meng³,
Li Lei⁴,
Sun Di⁵,
Liu Hui⁶

1.
School of Resources and Environment, University of Jinan, Jinan 250022, China
2.
Key Laboratory of Tectonics and Petroleum Resources, China University of Geosciences, Wuhan 430074, China
3.
No.1 Institute of Geology and Mineral Resources of Shandong Province, Jinan 250014, China
4.
China National Offshore Oil Corporation Ltd. Zhanjiang, Zhanjiang 524057, China
5.
Petroleum Development centre, Shengli Oilfield Company, SINOPEC, Dongying 257000, China
6.
Shandong Institute of Geophysical & Geochemical Exploration, Jinan 250013, China

摘要

摘要: 通过钻井、测井与地震数据，依据不整合面分析、断层活动速率分析与地层的"负向结构"分析，在义和庄凸起东部燕山期内识别出一期发生于中晚侏罗世之交的构造负反转，并据此将义和庄凸起燕山期划分为早期与晚期两个阶段.通过单井与连井层序地层分析，分别建立了燕山早期与晚期的层序地层样式，两者在层序结构及内部沉积充填等方面表现出巨大差异.早期层序地层不具有显著的沉积厚度分异，且格架内部充填河流相沉积；晚期因构造负反转而形成小型拉张断陷盆地，沉积厚度分异明显，内部以扇三角洲沉积充填为主，呈现出对构造负反转的显著响应.燕山期构造-层序地层学的研究可为中国东部其他具有相似构造背景盆地前新生代的油气勘探提供借鉴.
- 燕山期 /
- 构造不整合面 /
- 构造负反转 /
- 层序地层 /
- 沉积学
Abstract: Through boreholes, well logs and seismic profiles, one tectonic inversion happening between Middle Jurassic and Late Jurassic is recognized in Yanshanian eastern Yihezhuang salient based on analyzing unconformity surfaces, faulting activity and the negative structure of strata, which divides the Yanshanian of eastern Yihezhuang salient into Early Yanshanian and Late Yanshanian in this study. The sequence stratigraphic patterns of Early Yanshanian and Late Yanshanian are respectively established with analysis of single-well sequence stratigraphy and connecting-well sequence stratigraphy, which shows great difference in sequence structure and internal makeup with each other. During early Yanshanian, the sequence stratigraphy showed unobvious thickness differentiation and the sequence-infill were fluvial facies. Differently, the sequence stratigraphy presented obvious thickness differentiation and was infilled mainly with fan deltas, as the tectonic inversion led to development of small rifted-basin, which showed obvious response to the recognized tectonic inversion. Applying tectonic-sequence stratigraphy to Yanshanian succession could contribute to the pre-Cenezoic hydrocarbon exploration of the basins with similar tectonic background in eastern China.
- Yanshanian /
- tectonic unconformity /
- tectonic inversion /
- sequence stratigraphy /
- sedimentology

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图 2 渤海湾盆地济阳坳陷义和庄凸起东部地层划分与盆地充填演化

据张善文等(2009)修改

Fig. 2. The stratigraphic division and basin filling evolution of the eastern Yihezhuang salient, Jiyang depression, Bohai Bay basin

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图 3 义和庄凸起东部三维地震剖面层序界面识别

地震测线A-A′，位置见图 1

Fig. 3. Recognition of sequence boundaries (sb) on the 3D seismic profile across eastern Yihezhuang salient

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图 1 义和庄凸起东部构造位置与区域地质背景

a.渤海湾盆地位置; b.济阳坳陷在渤海湾盆地中位置; c.研究区位置

Fig. 1. Location and regional geologic background of eastern Yihezhuang salient

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图 4 钻井层序地层界面识别

a.Tmz3界面上下岩性、测井曲线等发生显著变化.界面以下为厚层泥岩夹薄层粉砂质沉积，测井曲线呈齿型，岩性变化较快; 界面之上为厚层砂岩沉积，测井曲线为箱型-钟型，为河道边滩沉积，对下伏地层造成冲刷；b.Tg界面之上为厚层含砾砂岩沉积, 测井曲线呈漏斗型-钟型, 为河道边滩沉积; 界面之下为泥岩与砂岩的薄互层, 测井曲线呈低幅齿型.Tg界面上下岩性、测井曲线形态发生显著变化.Tg为河道冲刷面，可构成层序界面；c.Tg界面上下最显著的差异是沉积物颜色发生明显变化，Tg界面之下为泥岩与砂岩薄互层沉积，并夹煤层，沉积物颜色为灰色，指示还原环境；界面之上为厚层泥岩夹薄层砂岩沉积，沉积物颜色为紫红色，指示氧化环境；井位置见图 1

Fig. 4. Recognition of sequence boundaries (sb) on boreholes

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图 5 济阳坳陷义和庄凸起东部燕山期层序地层格架

地震测线B-B′，位置见图 1

Fig. 5. Yanshanian sequence stratigraphic framework of eastern Yihezhuang salient, Jiyang depression

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图 6 义和庄凸起东部各构造不整合面的地震反射特征

地震测线C-C′，位置见图 1；Tg2.沉积基底；Tg.中生界底界面；Tgm.上侏罗统底界面；Tr.新生界底界面

Fig. 6. Characteristics of seismic reflections of tectonic unconformities in eastern Yihezhuang salient

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图 7 YG991断层活动速率及演化

Fig. 7. The evolution and active rate of Fault YG991

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图 8 义和庄凸起东部燕山期地层负向结构

a.坊子组与三台组(J₁+J₂)残余地层厚度; b.蒙阴组(J₃)残余地层厚度

Fig. 8. The negative structure of Yanshanian strata in eastern Yihezhuang salient

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图 9 D4单井层序地层分析

MFS.最大洪泛面; TS.初始洪泛面; SB.层序界面; LST.低位体系域; EST.扩展体系域; HST.高位体系域.井位置见图 1

Fig. 9. equence stratigraphic analysis of Well D4

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图 11 义和庄凸起东部燕山早期连井层序地层分析（岩性图例同图 10）

Fig. 11. Early Yanshanian sequence stratigraphic analysis of connecting-wells in eastern Yihezhuang salient

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图 10 D5单井层序地层分析

UST.削截型不整合面; TS.初始洪泛面; SB.层序界面; LST.低位体系域; EST.扩展体系域.井位置见图 1

Fig. 10. Sequence stratigraphic analysis of Well D5

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图 12 义和庄凸起东部燕山晚期连井层序地层分析（岩性图例同图 10）

Fig. 12. Late Yanshanian sequence stratigraphic analysis of connecting-wells in eastern Yihezhuang salient

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图 13 义和庄凸起东部燕山早期(坊子组与三台组同沉积期)垂向层序地层样式(岩性图例同图 10)

Fig. 13. Early Yanshanian (syndepositional period of Fangzi Formation and Santai Formation) vertical sequence stratigraphic patterns in eastern Yihezhuang salient

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图 14 义和庄凸起东部燕山晚期(蒙阴组同沉积期)垂向层序地层样式(岩性图例同图 10)

Fig. 14. Late Yanshanian (syndepositional period of Mengyin Formation) vertical sequence stratigraphic patterns in eastern Yihezhuang salient

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图 15 义和庄凸起东部燕山早期与燕山晚期横向层序地层样式

Fig. 15. Early and late Yanshanian horizontal sequence stratigraphic patterns in eastern Yihezhuang salient

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