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扇三角洲沉积体系高精度层序地层学研究
引用本文:赵俊青,纪友亮,夏斌,张善文,刘宝明.扇三角洲沉积体系高精度层序地层学研究[J].沉积学报,2004,22(2):302-309.
作者姓名:赵俊青  纪友亮  夏斌  张善文  刘宝明
作者单位:中国科学院广州地球化学研究所与南海海洋研究所,边缘地质重点实验室,广州,510640;同济大学海洋与地球科学学院,上海,200092;中国石油化工胜利油田有限公司,山东东营,257015
基金项目:国家科技攻关项目 , 国家重点基础研究发展计划(973计划)
摘    要:以东营凹陷胜北断层下降盘坨76块沙四上亚段扇三角洲沉积体为例,对扇三角洲沉积体系下的高精度层序地层学进行了研究。经过分析认为,在扇三角洲沉积体系中的高精度层序地层单元划分为准层序组、准层序、层组、层四级,并对准层序和层组的类型和对比方法进行了总结。将扇三角洲沉积体系中的层组类型划分为Fu、Cu和Cu-Fu三大类,准层序类型划分为Fu-Fu、Cu-Fu、Cu-Cu三大类,同时总结出了沿物源方向的相序递变和垂直物源方向的侵蚀切割对比2种准层序和层组对比模式。

关 键 词:扇三角洲  高精度层序地层学  准层序  层组  对比模式  沙四上亚段
文章编号:1000-0550(2004)02-0302-08
收稿时间:2003-02-10
修稿时间:2003年2月10日

High-Resolution Sequence Research in Fan-delta Sedimentary System
ZHAO Jun-qing,JI You-liang,XIN Bin,ZHANG Shan-wen,LIU Bao-ming.High-Resolution Sequence Research in Fan-delta Sedimentary System[J].Acta Sedimentologica Sinica,2004,22(2):302-309.
Authors:ZHAO Jun-qing  JI You-liang  XIN Bin  ZHANG Shan-wen  LIU Bao-ming
Institution:1.Laboratory of Marginal Sea Geology, Guangzhou Institute of Geochemistry & South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, 510640;2.Institute of Earth and Ocean Science, Tongji University, Shanghai 200092;3.Shengli Oil field Limited Corporation, SINOPEC, Dongying Shandong 257015
Abstract:This paper discusses high-resolution sequence in fan-delta sedmentary system, exemplifying T76 fan-delta of the fourth upper member of Shhejie formation in Shengbei fault's downthrown side of Dongying depression.Research shows that the high resolution sequence stratigraphic units are divided into parasequence set,parasequence,bed set and bed in fan-delta. The authors particularly study types and comparative methods of parasequence and bed set. The type of bed set is divided into Fu,Cu and Cu-Fu types, and parasequence into Fu-Fu,Cu-Fu and Cu-Cu types. We have summrized two comparative methods of parasequence and bed set which are facies change paralleling to source area and incisement perpendicular to the source area.
Keywords:fan-delta  high-resolution sequence stratigraphy  parasequence  bed set  comparative method  the fourth upper member of Shahejie Formation  
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