首页 | 本学科首页   官方微博 | 高级检索  
     检索      

准噶尔盆地阜东斜坡区中上侏罗统储集层特征差异及控制因素分析
引用本文:于景维,叶勇,柳妮,朱永才,文华国.准噶尔盆地阜东斜坡区中上侏罗统储集层特征差异及控制因素分析[J].地质学报,2018,92(5):1070-1080.
作者姓名:于景维  叶勇  柳妮  朱永才  文华国
作者单位:中国石油大学(北京)克拉玛依校区;中国石油新疆油田分公司勘探开发研究院;克拉玛依职业技术学院;成都理工大学"油气藏地质及开发工程"国家重点实验室
基金项目:国家自然科学基金项目(面上项目,重点项目,重大项目)
摘    要:准噶尔盆地是中国西部地区最重要的含油气盆地之一,阜东斜坡区中上侏罗统头屯河组和齐古组是近期勘探重点。根据野外露头、钻井岩芯和分析化验资料,详细分析头屯河组和齐古组储集层特征差异,包括储集层岩矿特征和物性特征差异。岩矿特征中重点对碎屑、填隙物以及孔隙类型和结构特征进行对比分析,物性特征中重点对储集层类型进行研究,发现齐古组储集砂层储集质量总体上要好于头屯河组。通过综合分析,认为阜东斜坡区中上侏罗统储集层特征差异主要受构造、沉积相、异常压力和成岩作用复合控制,构造演化的差异是导致头屯河组和齐古组储集层特征差异的最关键因素,头屯河组物性最好储集层的微相类型为水下分流河道,齐古组物性最好储集层的微相类型为分流河道,异常压力对原生孔隙保存以及黏土矿物发育位置起到重要影响,成岩作用对于重点层位储集层物性好坏起到决定性作用,其中凝灰质的蚀变序列对于后期油气开发有重要参考价值。

关 键 词:准噶尔盆地  阜东斜坡区  中上侏罗统  储集层特征  控制因素
收稿时间:2015/4/23 0:00:00
修稿时间:2018/4/19 0:00:00

Character Differences and Controlling Factors of Reservoirs in the Upper-Middle Jurassic Fudong Slope Area, Junggar Basin
YU Jingwei,YE Yong,LIU Ni,ZHU Yongcai and WEN Huaguo.Character Differences and Controlling Factors of Reservoirs in the Upper-Middle Jurassic Fudong Slope Area, Junggar Basin[J].Acta Geologica Sinica,2018,92(5):1070-1080.
Authors:YU Jingwei  YE Yong  LIU Ni  ZHU Yongcai and WEN Huaguo
Institution:1) Karamay Campus of China University of Petroleum, Karamay, Xinjiang, 834000,2) CNPC Xinjiang Oilfield Exploration and Development Research Institution, Karamay, Xinjiang, 834000,3) Karamay Vocational & Technical College, Karamay, Xinjiang, 834000,2) CNPC Xinjiang Oilfield Exploration and Development Research Institution, Karamay, Xinjiang, 834000 and 4) Chengdu University of Technology, Chengdu, 610059
Abstract:TheJunngar basin has been one of the most important petroliferous basins in western China. The Toutunhe and Qigu formations in the Upper Middle Jurassic Fudong slope area are the recent key strata for exploration. Based on field outcrop, drilling cores and analysis test data, character differences of reservoirs in the Toutunhe and Qigu formations were studied in detail using petrolgic characteristics and physical properties differences of reservoirs. For the former, comparative study was performed on clastic, interstitial material, pore types and structural characteristics, and for the latter, reservoir type is the focus. The study shows that reservoir quality of the Qigu formation is better than that of Toutunhe formation. Comparative analysis indicates that the character differences of reservoirs of Upper Middle Jurassic in study area are compositely controlled by tectonic, sedimentary facies, abnormal pressure and diagenesis, with tectonic evolution being the leading factor. The best microfacies responsible for good physical properties of the Toudunhe Formation is underwater distributary channel while the best that for the Qigu Formation is distributary channel. Abnormal pressures have important impact on preservation of primary pores and position of minerals development. Diagenesis plays a conclusive role in reservoir physical properties, with tuffaceous alteration sequence having important reference value for future exploration of oil and gas.
Keywords:Junngar basin  Fudong slope area  Upper Middle Jurassic  reservoir characters  controlling factors
本文献已被 CNKI 等数据库收录!
点击此处可从《地质学报》浏览原始摘要信息
点击此处可从《地质学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号