冀中坳陷饶阳凹陷古近系层序地层学及演化模式<sup>&#x0002A;</sup>

古地理学报 ›› 2006, Vol. 8 ›› Issue (3): 397-406.

• 层序地层学及古地理学 • 上一篇下一篇

冀中坳陷饶阳凹陷古近系层序地层学及演化模式^*

纪友亮¹, 杜金虎², 赵贤正³, 张以明³, 张瑞峰³

1 同济大学海洋与地球科学学院,上海 200082;
2 中国石油勘探与生产公司,北京 100724;
3 中国石油华北油田公司,河北任丘 062552

收稿日期:2006-02-08 修回日期:2006-02-28 出版日期:2006-06-01 发布日期:2006-06-01
作者简介:纪友亮,男,1962年10月生,同济大学海洋与地球科学学院教授,CNPC储层重点实验室副主任,博士生导师,现从事石油地质学、沉积学和层序地层学方面的科研和教学工作。通讯地址: 上海市四平路1239号同济大学海洋与地球科学学院,邮政编码: 200092;电话: 021-65985163; Email: jiyouliang@mail.tongji.edu.cn。
基金资助:
*本文是国家十五科技攻关项目研究成果的一部分,课题编号2004BA616A-04-02

Sequence stratigraphy and evolution models of the Paleogene in Raoyang Sag, Jizhong Depression

Ji Youliang¹, Du Jinhu², Zhao Xianzheng³, Zhang Yiming³, Zhang Ruifeng³

1 School of Ocean and Earth Science, Tongji University, Shanghai 200092;
2 PetroChina Exploration m Production Company,Beijing 100724;
3 PetroChina Huabei Oilfield Company, Renqiu 062552, Hebei

Received:2006-02-08 Revised:2006-02-28 Online:2006-06-01 Published:2006-06-01
About author:Ji Youliang, born in October, 1962, got his doctoral degree from Petroleum University (Beijing) in 1991. Now he is a professor in Tongji University, and a vice director of Key Lab of Reservoir of CNPC, and is mainly engaged in sedimentology, petroleum geology and sequence stratigraphy.

摘要/Abstract

摘要： 根据陆相地层层序在地震剖面和电测曲线上的识别标志、岩石类型组合特点以及古生物等方面的特征,将饶阳凹陷古近系划分出3个二级层序、10个三级层序。其中层序Ⅰ、Ⅱ为裂谷初始期湖泊层序,层序Ⅲ、Ⅳ、Ⅴ、Ⅵ、Ⅶ为裂谷强活动期湖泊层序,层序Ⅷ、Ⅸ、Ⅹ为河流层序。其中裂谷期湖泊层序可以划分为 3个体系域,即低位体系域、湖侵体系域和高位体系域,而河流层序可划分为基准面上升体系域和基准面下降体系域。针对研究区目的层段层序发育的特点,在层序地层单元划分和对比的基础上,结合构造发育史和地层厚度的变化所反映的古地形,建立了该区层序地层学演化模式,并初步分析了不同层序演化模式与油气的关系预测了不同层序的地层油藏。

关键词: 冀中坳陷, 饶阳凹陷, 古近系, 层序地层学, 演化模式

Abstract: Based on the identification features of continental stratigraphic sequences on seismic profiles and wire line logs, the characteristics of lithologic combination and palaeontology, the Paleogene in the Raoyang Sag is divided into three second order sequences and ten third order sequences. Third order sequences Ⅰand Ⅱ are lacustrine sequences developed in the initial rifting phase of basin formation, while sequences Ⅲ,Ⅳ,Ⅴ,Ⅵ and Ⅶ are lacustrine sequences developed in the strong rifting phase, and sequences Ⅷ,Ⅸ and Ⅹ are fluvial sequences. Lacustrine sequences can be divided into three system tracts: low stand, transgressive and high stand system tracts. Fluvial sequences can be divided into base level rising and base level falling system tracts. Based on the identification and correlation of sequence stratigraphic units, sequence stratigraphic models of the target strata in the study area are established according to the characteristics of the stratigraphic sequences, the tectonic evolution history and paleontography reflected by the variation of strata thickness. A preliminary analysis is made on the relationship between sequence stratigraphic models and oil gas exploration potentials, and the stratigraphic oil pools in each sequences are predicted/

Key words: Jizhong Depression, Raoyang Sag, Paleogene, sequence stratigraphy, evolution models

中图分类号:

P539.2

纪友亮, 杜金虎, 赵贤正, 张以明, 张瑞峰. 冀中坳陷饶阳凹陷古近系层序地层学及演化模式^*[J]. 古地理学报, 2006, 8(3): 397-406.

Ji Youliang, Du Jinhu, Zhao Xianzheng, Zhang Yiming, Zhang Ruifeng. Sequence stratigraphy and evolution models of the Paleogene in Raoyang Sag, Jizhong Depression[J]. JOPC, 2006, 8(3): 397-406.

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