鄂尔多斯盆地临兴地区石盒子组储层成岩作用研究

被引:0
作者
陈柏瑞
机构
[1] 中国石油大学(北京)
关键词
鄂尔多斯盆地; 石盒子组; 成岩作用; 成岩相; 储层特征;
D O I
暂无
年度学位
2016
学位类型
硕士
摘要
鄂尔多斯盆地临兴地区石盒子组致密储层油气显示良好,论文针对该储层开展了成岩作用研究,对认识及深入评价该构造带油气潜力具有重要意义。利用薄片鉴定、毛管压力、扫描电镜、阴极发光、X衍射分析、岩石热解、孢粉试验等分析测试手段,系统研究了鄂尔多斯盆地临兴地区石盒子组的成岩作用类型、成岩阶段、成岩序列及成岩相,探讨了储层物性影响因素。临兴地区石盒子组储层以中细砂岩为主,孔隙类型主要为次生孔隙,粒间溶蚀孔和粒内溶蚀孔发育。储层存在压实作用、胶结作用、交代作用和溶蚀作用,成岩阶段处于中成岩A期。储层成岩相包括压实压溶相、碳酸盐岩胶结相、胶结-弱溶蚀相、自生高岭石充填粒间孔相、次生溶孔相、原生孔+次生孔相六种类型,上石盒子组中储层物性较好的成岩相主要为次生孔相、原生孔相、高岭石充填粒间孔相与胶结弱溶蚀相,主要分布在盒2段、盒3段与盒4段。下石盒子组中次生孔相、原生孔+次生孔相、高岭石充填粒间孔相形成有力储层,主要分布在盒5段、盒6段与盒8段。临兴地区石盒子组储层物性与砂岩粒径、岩屑含量、长石含量呈正比关系,与石英含量、碳酸盐含量呈反比关系。储层物性变差主要受压实作用影响,其次受胶结作用控制。原生孔+次生溶孔相带及次生溶孔相带孔渗性最好,压实压溶相带和碳酸盐胶结相带孔渗性最差。
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页数:71
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