岩性油气藏 ›› 2010, Vol. 22 ›› Issue (1): 43–47.doi: 10.3969/j.issn.1673-8926.2010.01.008

• 油气地质 • 上一篇    下一篇

鄂尔多斯盆地盐定地区三叠系延长组长2 油层组沉积相研究

陈斐1,魏登峰2,余小雷1,吴少波1   

  1. 1.西安石油大学油气资源学院; 2.延长油田股份有限公司七里村采油厂
  • 出版日期:2010-03-15 发布日期:2010-03-15
  • 作者简介:陈斐,1986 年生,女,西安石油大学在读硕士研究生,研究方向为矿产普查与勘探。地址:(710065)陕西省西安市电子二路18# 西 安石油大学油气资源学院46# 信箱。E-mail:284558180@qq.com

Sedimentary facies of Chang 2 oil-bearing member of Yanchang Formation in Yanchi-Dingbian area, Ordos Basin

CHEN Fei1,WEI Dengfeng2,YU Xiaolei1,WU Shaobo1   

  1. 1. School of Petroleum Resources, Xi’an Shiyou University, Xi’an 710065, China; 2. Qilicun Oil Production Plant, Yanchang Oilfield Company Ltd., Yan’an 717100, China
  • Online:2010-03-15 Published:2010-03-15

摘要:

根据大量的钻井、测井及分析化验资料,运用沉积学方法综合研究该区的沉积相及其演化特征,并认为:长2 油层组早、中期(长23、长22)主要发育曲流河沉积,表现为垂向上河道砂体相互叠加,砂地比值高,平面上河道沉积广泛分布,泛滥平原沉积保存较少;晚期(长21)过渡为网状河沉积,河道砂体厚度变薄,地层砂地比变小,平面上河道呈网状分布,广泛发育河漫沼泽沉积。在沉积单元划分、对比的基础上,分析了4 个单元沉积微相的平面展布规律。

关键词: 水下扇;储层特征;控制因素, 双阳组;莫里青断陷

Abstract:

Based on drilling cores and logging data, the sedimentary facies and its evolution characteristics of Chang 2 oil-bearing member in Yanchi-Dingbian area, Ordos Basin are studied. The result shows that fluvial system developed in Chang 2 depositional stage in this region. During the depositional period, there is a systematic change in channel types from meandering stream to anastomosing river. The meandering stream deposition developed at the bottom and middle sections (Chang 23, Chang 22) ofChang 2 member with thicker superposed channel sand body, higher sand-stone/ stratum ration, less floodplain and more channel deposits. While the anastomosing river deposition developed at the top section (Chang 21) of Chang 2 member with thinner channel sandstone-body, lower sandstone/stratum ration, less channel and more floodplain, swamp deposits. On the basis of sedimentary units division and correlation, the microfacies plane distributions of the 4 units are analyzed.

Key words: subaqueous fan, reservoir characteristics, controlling factor, Shuangyang Formation, Moliqing Fault Depression

[1] 长庆油田石油地质志编写组.中国石油地质志(卷十二)[M].北京:石油工业出版社,1992.
[2] 何自新.鄂尔多斯盆地演化与油气[M].北京:石油工业出版社,2003.
[3] 喻建,韩永林,凌升阶.鄂尔多斯盆地三叠系延长组油田成藏地质特征及油藏类型[J].中国石油勘探,2001,6(4):13-19.
[4] 杨华,付金华,喻建.陕北地区大型三角洲油藏富集规律及勘探技术应用[M].石油学报,2003,24(3):6-10.
[5] 刘化清,袁剑英,李相博,等. 鄂尔多斯盆地延长期湖盆演化及其成因分析[J].岩性油气藏, 2007,19(1):52-56.
[6] 沉积构造与环境解释编著组.沉积构造与环境解释[M].北京:科学出版社,1982.
[7] 梅志超,彭荣华,杨华,等. 陕北上三叠统延长组含油砂体的沉积环境[J].石油与天然气地质,1989,9(3):261-267.
[8] 曾少华. 陕北三叠系延长统湖盆三角洲沉积模式的建立[J].石油与天然气地质,1992,13(2):227-235.
[9] 陈永峤,靳文奇,文志刚,等. 靖安油田张渠一、二区长213 沉积微相研究[J].岩性油气藏,2008,20(4):43-46.
[10] 石雪峰,杜海峰.姬塬地区长3—长4+5 油层组沉积相研究[J].岩性油气藏,2008,20(1):59-63.
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