地质科学
     首页 | 过刊浏览 |  本刊介绍 |  编委会 |  投稿指南 |  期刊征订 |  留言板 |  批评建议 |  联系我们 |  English
地质科学  2002, Vol. Issue (2): 219-230    DOI:
论文 最新目录 | 下期目录 | 过刊浏览 | 高级检索  |   
胜利油田孤岛油区馆陶组上段沉积结构单元
李阳1, 李双应2, 岳书仓2, 王忠诚3, 李忠3, 吴朝东4, 李翔3
1. 胜利石油管理局, 山东, 东营, 257001;
2. 合肥工业大学资源与环境科学系, 合肥, 230009;
3. 中国科学院地质与地球物理研究所, 北京, 100029;
4. 北京大学地质学系, 北京, 100871
SEDIMENTARY ARCHITECTURAL ELEMENTS OF UPPER MEMBER OF THE GUANTAO FORMATION IN GUDAO AREA, SHENGLI OILFIELD
Li Yang1, Li Shuangying2, Yue Shucang2, Wang Zhongcheng3, Li Zhong3, Wu Chaodong4, Li Xiang3
1. Shengli Petroleum Administration, Dongying, Shandong 257001;
2. Department of Natural Resources and Environmental Sciences, Hefei University of Technology, Hefei 23000;
3. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029;
4. Department of Geology, Peking University, Beijing 1000871
 全文: PDF (1550 KB)   HTML( )   输出: BibTeX | EndNote (RIS)      背景资料
摘要 结构单元分析法(Architectural-Element Analysis)作为一种比较成熟的研究方法,已广泛应用于古代河流沉积研究.本文首次根据钻孔资料分析胜利油田孤岛油区馆陶组上段5~1+2砂层组河流沉积的结构单元.该段5~1+2砂层组岩石类型简单,可分为11个岩相类型.根据界面特征、岩相组合、内部几何形态、外部几何形态和垂向剖面特征等划分出6个结构单元:河道滞流沉积(CHL)、侧向加积砂坝(LA)、天然堤(LV)、决口扇(CS)、决口水道(CR)和洪泛平原细粒(FF).其中洪泛平原细粒(FF)、决口扇(CS)和侧向加积砂坝(LA)结构单元最为发育,其次是天然堤(LV)和决口水道(CR)结构单元,而河道滞流沉积(CHL)结构单元则不甚发育.决口扇(CS)结构单元是馆陶组上段砂体发育的主要单元之一,且富含油气资源.因此,进一步加强决口扇的研究对油气资源的勘察是十分必要的.
服务
把本文推荐给朋友
加入我的书架
加入引用管理器
E-mail Alert
RSS
作者相关文章
李阳
李双应
岳书仓
王忠诚
李忠
吴朝东
李翔
关键词岩相类型   结构单元   河流沉积   馆陶组上段   孤岛油区   胜利油田     
Abstract: Architectural element analysis advanced by Miall, as a relative common method, has been extensively applied on studying ancient fluvial deposits in the world. Based on the drill data, this paper studied, firstly, the architectural elements of fluvial deposits of the 5~1+2 sandstones in the Upper Members of Guantao Formation (UMGF) in the Gudao area, Shengli Oilfeild. There are 11 kinds of petrofacies in the 5~1+2 sandstones of the UMGF, with simple rock association. On the basis of bounding surface features, petrofacies assemblage, internal geometry, external form and vertical profile, etc., the sandstones can be divided into 6 architectural elements, namely, the channel lag (CHL), the lateral accretion macroform (LA), the levee (LV), the crevasse splay (CS), the crevasse channel (CR) and the floodplain fines (FF), in which the architectural elements of FF, CS and LA develop extensively, the LV and CS occur subordinately, and the CHL develops poorly. The crevasse splay element is one of architectural elements which, as a main unit of sand bodies in the UMGF, contains rich oil and gas. It is necessary to make more study on the element of crevasse splay for exploration of oil and natural gas.
Key wordsPetrofacies   Architectural elements   Fluvial deposits   the Upper Member of Guantao Formation   Gudao area   Shengli Oilfield.   
收稿日期: 2001-07-09;
引用本文:   
李阳,李双应,岳书仓等. 2002, 胜利油田孤岛油区馆陶组上段沉积结构单元. 地质科学, (2): 219-230.
Li Yang,Li Shuangying,Yue Shucang et al. SEDIMENTARY ARCHITECTURAL ELEMENTS OF UPPER MEMBER OF THE GUANTAO FORMATION IN GUDAO AREA, SHENGLI OILFIELD[J]. Chinese Journal of Geology, 2002, (2): 219-230.
 
没有本文参考文献
[1] 童亨茂, 郑磊. 三维地震资料在古应力场反演和裂缝预测中的应用——以胜利油田富台潜山为例[J]. 地质科学, 2007, (1): 45-57.
[2] 高德章, 赵金海, 薄玉玲, 唐建. 东海及邻近地区岩石圈三维结构研究[J]. 地质科学, 2006, (1): 10-26.
[3] 吴朝东, 刘建民, 王军, 李忠, 谢小建. 河流沉积单元分析与储层宏观非均质性[J]. 地质科学, 2003, (1): 60-73.
[4] 王俊玲, 任纪舜. 嫩江现代河流沉积体岩相及内部构形要素分析[J]. 地质科学, 2001, (4): 385-394.
[5] 赫英, 王定一, 廖永胜. 胜利油田火山岩类、盆地演化及其CO2-Au成藏成矿效应[J]. 地质科学, 2001, (4): 454-464.
[6] 赫英, 朱兴国, 徐培苍. 胜利油田火山岩单个包裹体碳同位素[J]. 地质科学, 1998, (3): 380-383.
[7] 陈代钊. 河流沉积占优势地层中高频层序地层——以贵州盘县西部龙潭组为例[J]. 地质科学, 1997, (4): 432-444.
 
版权所有 © 2009-2017 《地质科学》编辑部
地址:北京9825信箱  邮政编码:100029
电话:010-82998109  010-82998115
京ICP备05029136号-10