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近岸水下扇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,任拥军,张善文.近岸水下扇沉积体系高精度层序地层学研究[J].沉积学报,2005,23(3):490-497.
作者姓名:赵俊青  纪友亮  夏斌  任拥军  张善文
作者单位:1.中国科学院广州地球化学研究所与南海海洋研究所边缘海地质重点实验室,广州 510640;
基金项目:国家重点基础研究发展计划(973计划) , 国家科技攻关项目 , 中国科学院知识创新工程项目
摘    要:以东营凹陷胜北断层下降盘坨85块沙河街组沙三中亚段近岸水下扇沉积体为例,对近岸水下扇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,近岸水下扇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。将近岸水下扇积体系中的层组类型划分为Fu(Fineup)、Cu(Coareseup)和Hu(Homogenicup)三大类,准层序类型划分为Cu-Fu、Cu-Cu、Cu-Hu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种准层序对比模式和侵蚀叠置、相变对比、薄砂层对比、相似渐变等4种层组对比模式。

关 键 词:近岸水下扇    高精度层序地层学    准层序    层组    沙三中亚段
文章编号:1000-0550(2005)03-0490-08
收稿时间:2004-07-06
修稿时间:2004-11-23

High-Resolution Sequence Research on Nearshore Subaqueous Fan System
ZHAO Jun-qing,JI You-liang,XIA Bin,REN Yong-jun,ZHANG Shan-wen.High-Resolution Sequence Research on Nearshore Subaqueous Fan System[J].Acta Sedimentologica Sinica,2005,23(3):490-497.
Authors:ZHAO Jun-qing  JI You-liang  XIA Bin  REN Yong-jun  ZHANG Shan-wen
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.Institute of Earth Resource and Information, University of Petroleum China, Dongying Shandong 257061;4.Shengli Oil Field Limited Corporation, SINOPEC, Dongying Shandong 257015
Abstract:This paper discusses the high-resolution sequence in nearshore subaqueous fans sedimentary system, exemplifying T85 nearshore subaqueous fans of the third middle member of Shhejie Formation in Shengbei fault's downthrown side of Dongying depression. The research shows that the high-resolution sequence stratigraphic units are divided into parasequence set, parasequence, bed set and bed in the fan-delta.Types and comparison methods of parasequence and bed set are especially studied. The type of bed set is divided into Fu, Cu and Hu, and parasequence into Cu-Fu, Cu-Fu and Cu-Hu. Two comparison methods of parasequence are provided that are facies change paralleling to source area and incision perpendicular to source area and four models of bed set which are correlation of overstacking, correlation of facies change, correlation of thin sandstone bed and correlation of similar changing of lithology.
Keywords:nearshore subaqueous fan  high-resolution sequence stratigraphy  parasequence  bed set  the third middle member of Shahejie Formation
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