特种油气藏2024,Vol.31Issue(6) :67-76.DOI:10.3969/j.issn.1006-6535.2024.06.008

准噶尔盆地齐古组浅水河控三角洲沉积特征及模式探讨

Sedimentary Characteristics and Models of Shallow-Water River-Dominated Delta in Qigu Formation,Junggar Basin

张美 任新成 商丰凯 徐佑德 曲彦胜
特种油气藏2024,Vol.31Issue(6) :67-76.DOI:10.3969/j.issn.1006-6535.2024.06.008

准噶尔盆地齐古组浅水河控三角洲沉积特征及模式探讨

Sedimentary Characteristics and Models of Shallow-Water River-Dominated Delta in Qigu Formation,Junggar Basin

张美 1任新成 1商丰凯 1徐佑德 1曲彦胜1
扫码查看

作者信息

  • 1. 中国石化胜利油田分公司,山东 东营 257000
  • 折叠

摘要

准噶尔盆地腹部A区上侏罗统齐古组是近年来油气勘探的热点地区,多口钻井获得了高产油气流,展示了较大的油气资源潜力.针对齐古组浅水三角洲前缘沉积体系有利砂体分布控制因素及模式不清等问题,综合岩心、测井、地震、重矿物及微量元素等资料,对研究区齐古组浅水河控三角洲沉积特征展开研究.研究表明:浅水河控三角洲形成于多物源供给、水体较浅且频繁震荡、水动力中等的沉积环境,砂体类型以河坝复合体为主,岩石普遍为氧化色.根据砾石层厚度、粒径、层理规模等将河坝复合体划分为主水道+残余河口坝、分支水道+残余河口坝、残余河口坝为主3类.其中,分支水道+残余河口坝、残余河口坝为主的河坝复合体为有利砂体,其分布主要受控于基准面变化、河道供源与古地貌、河流与波浪作用影响.有利砂体纵向上分布在基准面上升的中期;平面上分布在与主水道距离适中的斜坡区和平台区.该研究成果深化了浅水河控三角洲沉积特征研究,可为下一步优选区带提供依据,也可为类似区块提供借鉴.

Abstract

The Upper Jurassic Qigu Formation in Area-A within the hinterland of Junggar Basin is a hotspot for oil and gas exploration in recent years.Numerous wells have achieved high-yield oil and gas flows,demonstrating sig-nificant potential for oil and gas resources.In light of the sedimentary system of the shallow water delta front in the Qigu Formation,the controlling factors and patterns of favorable sand body distribution remain unclear.Based on the data of core,logging,seismic,heavy minerals and trace elements,the sedimentary characteristics of the shallow water river-controlled delta in the Qigu Formation within the study area are investigated.The study reveals that the river-controlled shallow-water delta is formed in a sedimentary environment characterized by multi-source supply,a shal-low water body,frequent oscillations,and a medium hydrodynamic force.The predominant sand body type is mainly the river-bar complex,and the rock is generally oxidized.Based on the thickness,particle size and bedding scale of gravel,the river dam complex is categorized into three types:main channel+residual mouth bar,branch channel+re-sidual mouth bar and residual mouth bar.Among them,the branch channel+residual mouth bar and the river dam complex dominated by residual mouth bar constitute favorable sand bodies.Their distribution is mainly governed by the variation of base level,the influence of river channel supply,ancient landform,river and wave.Favorable sand bodies are vertically distributed in the middle section of the base level rise;on the plane,they are distributed in the slope area and platform area at a moderate distance from the main channel.The research outcomes have deepened the investigation of the sedimentary characteristics of river-controlled shallow-water delta,offering a foundation for the subsequent optimization of the zone and also furnishing a reference for similar blocks.

关键词

浅水河控三角洲/沉积环境/砂体类型/沉积模式/准噶尔盆地

Key words

river-controlled shallow-water delta/sedimentary environment/sand body type/sedimentary model/Junggar Basin

引用本文复制引用

出版年

2024
特种油气藏
中油辽河油田公司

特种油气藏

CSTPCDCSCD北大核心
影响因子:1.626
ISSN:1006-6535
段落导航相关论文