沙垒田凸起前古近系基岩分布及源—汇过程

刘强虎; 朱筱敏; 李顺利; 李慧勇; 石文龙

doi:10.3799/dqkx.2016.134

沙垒田凸起前古近系基岩分布及源—汇过程

doi: 10.3799/dqkx.2016.134

刘强虎^1,2,,
朱筱敏^1,2, ,,
李顺利^1,2,
李慧勇³,
石文龙³

1.
中国石油大学油气资源与探测国家重点实验室，北京 102249
2.
中国石油大学地球科学学院，北京 102249
3.
中海石油(中国)有限公司天津分公司，天津 300452

基金项目:

国家自然科学基金项目 41272133

详细信息

作者简介:
刘强虎(1988-)，男，博士研究生，从事层序地层学及地震沉积学研究.E-mail: lqhchkd@163.com

通讯作者:
朱筱敏, E-mail: xmzhu@cup.edu.cn

中图分类号: P618.130
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出版历程
- 收稿日期: 2016-05-23
- 刊出日期: 2016-11-15

Pre-Palaeogene Bedrock Distribution and Source-to-Sink System Analysis in the Shaleitian Uplift

Liu Qianghu^{1,2
,},
Zhu Xiaomin^{1,2
, ,},
Li Shunli^1,2,
Li Huiyong³,
Shi Wenlong³

1.
State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249, China
2.
College of Geosciences, China University of Petroleum, Beijing 102249, China
3.
Tianjin Branch of China National Offshore Oil Corporation Limited, Tianjin 300452, China

摘要

摘要: 沙垒田凸起及围区凹陷是一个完整的源-汇系统.基于钻井岩心、三维地震及锆石测年等资料，刻画了沙垒田凸起前古近系基岩组成及分布并探讨了古近纪早期源-汇体系配置关系.研究表明，沙垒田凸起自南向北依次发育太古界-元古界混合花岗岩、奥陶-寒武系碳酸盐岩与碎屑岩、中生界火山碎屑岩；其中，凸起东段以元古代混合花岗岩为主，西段以奥陶-寒武系碳酸盐岩为主.结合古地貌可知，砂岩富集区与源-汇耦合系统相对应，即基岩组成、汇水区、物源通道及边界样式共同控制沉积砂体组成样式与规模.对比分析凸起东西段、南北侧各控制要素与沉积砂体间关联性，可知凸起东段南侧混合花岗岩基底、较大的汇水面积与物源通道及斜坡带对应高效源-汇系统.
- 基岩 /
- 源-汇体系 /
- 锆石定年 /
- 古地貌 /
- 沙垒田凸起 /
- 沉积学
Abstract: During the early stage of the Palaeogene, the Shaleitian uplift and its surrounding areas constituted a complete source-to-sink system. In this paper, we analysze the characteristics of Pre-Palaeogene bedrocks and sediment-dispersal patterns of the source-to-sink systems based on detritus, thin section, zircon and integrated seismic-logging data analysis. The results show that the Shaleitian uplift was filled by Archeozoic and Proterozoic metamorphic rock sediments, and Lower Palaeozoic carbonate rocks stacked with southward Mesozoic igneous rocks. The bedrocks mainly consist of Proterozoic metamorphic rocks in the southern part of eastern Shaleitian uplift, while the Lower Palaeozoic carbonate rocks in the northern part of western Shaleitian uplift. Based on the palaeogeomorphology, it is found a sand-rich area corresponds to a complete source-to-sink coupling system in the rift basin, and the stacked style and size of sandbodies in the sink are jointly controlled by the composition of bedrocks, catchment areas, sediment-transport pathways, fracture system and detritus accommodation space. It is concluded thateffective source-to-sink systems are mainly located in the southern part of the eastern Shaleitian uplift through comparative analysis of the coupling relationship among the various controls with sandbodies properties in the Shaleitian uplift and surrounding areas.
- bedrocks /
- source-to-sink system /
- zircon U-Pb ages /
- Paleogeomorphic /
- Shaleitian uplift /
- sedimentology

HTML全文

图 1 渤海湾盆地沙垒田凸起区域构造位置

Fig. 1. Tectonic location map of Shaleitian uplift in Bohai bay basin

下载: 全尺寸图片幻灯片

图 2 渤海湾盆地前古近系基底地层综合图

据徐长贵(2007)修改

Fig. 2. Generalised stratigraphic column of the Pre-Palaeogene basement in Bohai bay basin

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图 3 渤海湾盆地沙垒田凸起区基岩岩性及其微观组成特征

Pl.斜长石；Bi.黑云母；Q.石英；Mi.微斜长石；Pe.条纹长石

Fig. 3. Bedrock lithologic and its micro characteristics in the Shaleitian uplift, Bohai bay basin

下载: 全尺寸图片幻灯片

图 4 渤海湾盆地沙垒田凸起区前古近系基岩锆石U-Pb年龄分布特征

Fig. 4. Zircon U-Pb ages distribution from the Pre-Palaeogene bedrocks in the Shaleitian uplift, Bohai bay basin

下载: 全尺寸图片幻灯片

图 5 渤海湾盆地沙垒田凸起区前古近系基岩地震相类型及分布

Ar.太古界；Mz.中生界；O+.奥陶-寒武系；Pt.元古界

Fig. 5. Seismic facies types of the Pre-Palaeogene bedrocks and its distribution in the Shaleitian uplift, Bohai bay basin

下载: 全尺寸图片幻灯片

图 6 渤海湾盆地沙垒田凸起区前古近系连井-地震相特征

地震剖面位置见图 1

Fig. 6. Connecting-well section and seismic facies characteristics of the Pre-Palaeogene bedrocks in the Shaleitian uplift, Bohai bay basin

下载: 全尺寸图片幻灯片

图 7 渤海湾盆地沙垒田凸起前古近系基岩分布(a)及南北侧(b, c)输导体系分布

Fig. 7. Paleogeomorphology showing bedrock distribution characteristics of Pre-Palaeogene (a) and sediment-transport pathways (b, c) in the early stage of Paleogene, Shaleitian uplift, Bohai bay basin

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图 8 渤海湾盆地沙垒田凸起区古近纪早期源汇配置关系(a)及汇区典型地层切片(b)与镜下薄片分析(c)

Cal.方解石；Q.石英；Ser.绢云母；(+).正交光；(-).单偏光

Fig. 8. Sediment-dispersal patterns of source-to-sink systems (a), representative strata slice (b) and thin sections analysis (c) in the early stage of Paleogene, Shaleitian uplift, Bohai bay basin

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图 9 渤海湾盆地沙垒田凸起及围区古近纪早期源-渠-汇配置关系

Fig. 9. Sediment-dispersal patterns of source-to-sink systems for the early stage of Paleogene in the Shaleitian uplift and surrounding areas, Bohai bay basin

下载: 全尺寸图片幻灯片

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