您当前的位置:首页>论文资料>穆尼盆地第四纪深水弯曲水道:沉积构型、成因及沉积过程

穆尼盆地第四纪深水弯曲水道:沉积构型、成因及沉积过程

资料类别:论文资料

文档格式:PDF电子版

文件大小:6.41 MB

资料语言:中文

更新时间:2024-12-19 13:38:39



推荐标签:

内容简介

穆尼盆地第四纪深水弯曲水道:沉积构型、成因及沉积过程 第26卷
第2期
2012年4月
代地质现
GEOSCIFNCE
穆尼盆地第四纪深水弯曲水道:沉积构型、成因及沉积过程
李磊,邵子玮,都鹏燕,徐继璞(西安石油大学油气资源学院,陕西西安710065)
Vol. 26
No.2 4pr. 2012
摘要:深水水道是陆坡沉积的重要组成单元,深水水道储层受到广泛关注。基于高分辨率三维地震资料,利用地震属性、分频技术等研究穆尼盆地第四纪深水弯曲水道的沉积构型、成因及沉积过程,主要取得以下3个方面的成果:(1)建立了深水弯曲水道沉积构型模式。弯曲深水水道由水道和堤岸组成。堤岸脊将堤岸分成内堤岸和外堤岸两部分。水道由底部粗粒滞留沉积、深海泥质披覆沉积以及滑块组成。(2)深水水道早期为低考曲水道,后期逐渐演化为高弯曲水道。(3)建立了深水曲水道沉积的岩相模式,深水考曲水道由垂向加积水道和侧向迁移水道组成。顺重力流方向,侧向迁移带,内弯带以沉积作用为主,外李带以侵蚀作用为主。垂向加积带,水道底部相粒滞留沉积往往表现为垂向加积
待征。深水弯曲水道岩相模式的建立对深水浊积水道储层准确预测具有重要的理论指导意义。关键调:深水弯曲水道;沉积构型:沉积过程;岩相模式;穆尼盆地
中图分类号:TE121.3
文献标志码:A
文章编号:10008527(2012)02034906
QuaternarySinuousSubmarineChannelinMuniBasin
Architecture,GenesisandProcess LI Lei, SHAO Zi-wei, DU Peng-yan, XU Ji-pu
(School of Peroleum Resourees, Xi'an Shiyou Unitersity, Xian, Shaanxi, 710065, China)
Abstract: Submarine channels are important components of continental slope. Great attentions are attached to deep-water channel reservoirs, Based on the high resolution 3-D seismic data, seismic attribute and SpecDe-comp are used to study the architecture, genesis and process of the Quatemary submarine channels in Muni ba-sin. There are three main conclusions: (1) Model of sedimentary architecture in sinuous submarine channels are built in this paper. Submarine channels are composed of channel and levee. Channels can be divided into two parts by levee crest: inner levee and outer levee. Channel fills are consisted of the coarse lag, hemipelagic mud drape deposits and slide,(2)The evolution process of submarine channel has been summaried. In the ear-ly stage, submarine channel is characterized by low sinuous channel, and in the later stage, by high sinuousity.(3) Lithofacies models of sinuous submarine channel are established in this paper. Sinuous submarine channels are composed of migration channel and aggradation channel. Along gravity-flow channel, the inner concave is mainly sedimentation while the outer gives priority to erosion process. Coarse channel-lag deposits are character-ized by aggradation. Lithofacies model of sinuous submarine channel is an important theoretical significant for accurate reservoir prediction of deepwater turbidity.
Key words: sinuous submarine channel; architecture; sedimentary process; lithofacies model; Muni basin
收稿日期:20110920;改图日期:2011-12-25:责任编辑:孙义梅。
基金项目:国家"973"计划项目(2009CB219407);国家自然科学基金项日(40572067)。
作者简介:李磊,男,讲师,博士,1979年出生,地质资源与地质工程专业,主要从事深水沉积及储层预测研究。
Emsil; lilei002@ yahoo com ene
上一章:姚家岭地区重力场视密度三维反演应用 下一章:水中腐植酸现场快速检测方法实验研究

相关文章

深水单向迁移水道-堤岸沉积体系特征及形成过程 沉积盆地的成因地层分析 珠江口盆地荔湾井区珠江组深水扇沉积特征 松辽盆地民东地区地层划分及沉积环境 松辽盆地梨树断陷层序地层格架及沉积体系分布 沉积盆地构造热演化史研究及应用:以塔里木盆地东北缘孔雀河地区为例 祁连山及邻区第四纪地层区划与沉积序列 中国及邻区沉积盆地群结构与构造演化探讨——来自长剖面的研究对比