[an error occurred while processing this directive] 世界地质 2018, 37(4) 1206-1220,1225 DOI:   10.3969/j.issn.1004-5589.2018.04.020  ISSN: 1004-5589 CN: 22-1111/P

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本文关键词相关文章
柳河盆地
鹰嘴砬子组
沉积微相
储层
本文作者相关文章
蓝艺植
许中杰
程日辉
刘国东
刘华
宋立斌
PubMed
Article by Lan Y
Article by Xu Z
Article by Cheng R
Article by Liu G
Article by Liu H
Article by Song L
柳河盆地早白垩世鹰嘴砬子组沉积及储层发育特征
蓝艺植1, 许中杰1, 程日辉1, 刘国东2, 刘华2, 宋立斌2
1. 吉林大学地球科学学院, 长春 130061;
2. 吉林油田公司勘探开发研究院, 吉林 松原 138000
摘要: 柳河盆地是受走滑张扭-走滑压扭机制控制的转换伸展盆地。本文以钻井和典型露头剖面为基础,利用成分粒度分析、铸体薄片、扫描电镜、阴极发光及压汞测试等方法,研究鹰嘴砬子组沉积及储层特征。柳河盆地鹰嘴砬子组湖相、扇三角洲相和火山岩相发育,湖盆内碎屑沉积物主要来自盆地西侧和东南侧边缘。盆地内储层的孔渗条件较差,溶蚀和溶解作用对储层起到建设作用,压实和压溶作用、碳酸盐岩的胶结-交代作用、石英的次生加大以及充填作用对储层起到破坏作用。用于物性测试的储层孔渗条件欠佳,整体为Ⅳ类储层。但野外剖面出现的油迹表明鹰嘴砬子组曾发生油气的运移与聚集,显示该盆地存在有致密储层和油气藏,具有油气勘探的潜力。
关键词 柳河盆地   鹰嘴砬子组   沉积微相   储层  
Sedimentary and reservoir developmental characteristics of Early Cretaceous Yingzuilazi Formation in Liuhe Basin
LAN Yi-zhi1, XU Zhong-jie1, CHENG Ri-hui1, LIU Guo-dong2, LIU Hua2, SONG Li-bin2
1. College of Earth Sciences, Jilin University, Changchun 130061, China;
2. Exploration and Development Research Institute, Jilin Oilfield Company, Songyuan 138000, Jilin, China
Abstract: Liuhe Basin is a transform-extension basin, which is controlled by strike-slip transtensional and strike-slip compressional mechanism. Using the particle size analysis, casting sheet, scanning electron microscope, cathode luminescence and mercury injection, the authors study sedimentary and reservoir characteristics of Yingzuilazi Formation based on drilling data and outcrops. Lacustrine facies, fan delta facies and volcanic facies were developed in Yingzuilazi Formation, Liuhe Basin, and the detrital sediments in the lake basin are mainly from the western and southeastern margin of the basin. Reservoir porosity and permeability are poor in the basin. Dissolution improved reservoir properties, whereas compaction and pressure dissolution, cementation and metasomatism of carbonate, secondary growth of quartz and filling play destructive role on reservoir. The pore and permeability of the reservoir used for physical property testing are poor, and is classified as type Ⅳ reservoir. However, the oil trace in the outcrops indicates that oil and gas migration and accumulation of oil and gas occurred in Yingzuilazi Formation. It shows that there are tight reservoirs in the basin, which have the potential for oil and gas exploration.
Keywords: Liuhe Basin   Yingzuilazi Formation   sedimentary microfacies   reservoir  
收稿日期 2018-05-09 修回日期 2018-07-16 网络版发布日期  
DOI: 10.3969/j.issn.1004-5589.2018.04.020
基金项目:

国家自然科学基金项目(41872101)、国家青年科学基金项目(41402087)、中国博士后科学基金项目(2013M530976)联合资助.

通讯作者: 许中杰(1984-),男,副教授,研究生导师,主要从事构造沉积学与海洋地质学研究.E-mail:zhongjiexu@jlu.edu.cn
作者简介:
作者Email: zhongjiexu@jlu.edu.cn

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