| 三塘湖盆地火山岩中沸石的成因及其储层意义 |
| |
| 引用本文： | 梁浩,罗权生,孔宏伟,范谭广,任忠跃,郭克诚.三塘湖盆地火山岩中沸石的成因及其储层意义[J].沉积学报,2011,29(3):537-543. |
| |
| 作者姓名： | 梁浩 罗权生 孔宏伟 范谭广 任忠跃 郭克诚 |
| |
| 作者单位： | 中国地质大学 资源学院 武汉 430074 |
| |
| 摘 要： | 三塘湖盆地火山岩中沸石分布广泛,石炭系-上二叠统火山岩储层发育层系主要为哈尔加乌组、卡拉岗组、条湖组.储层储集空间类型以次生溶蚀孔缝为主,构造裂缝型和不整合面溶蚀为辅.通过对研究区内所选井的岩石组分统计,发现火山岩岩性以中基性熔岩为主,杏仁体较发育,杏仁充填孔中以沸石类易溶矿物为主,为后期溶蚀作用的发生创造了条件.研究...
|
| 关 键 词： | 火山岩 浊沸石 溶蚀作用 油气富集 |
| 收稿时间： | 1900-01-01 |
Formation and Distribution of Zeolite in Volcanic Rock and Its Effect on Reserviors in Santanhu Basin |
| |
| LIANG Hao,LUO Quang-sheng,KONG Hong-wei,FAN Tan-guang,REN Zhong-yue,GUO Ke-cheng.Formation and Distribution of Zeolite in Volcanic Rock and Its Effect on Reserviors in Santanhu Basin[J].Acta Sedimentologica Sinica,2011,29(3):537-543. |
| |
| Authors: | LIANG Hao LUO Quang-sheng KONG Hong-wei FAN Tan-guang REN Zhong-yue GUO Ke-cheng |
| |
| Institution: | School of Resources, China University of Geology, Wuhan 430074 |
| |
| Abstract: | The zeolite are widely distributed in volcanic rocks of Santanghu Basin,and the main groups developed in volcanic reservoirs of Carboniferous-Upper Permian strata are Haerjiawu Group,Kalagang Group,Tiaohu Group.The types of reservoir space are mostly secondary dissolution aperture,with tectoclase and unconformity dissolution secondarily.Based on the study of the rock composition statistics of the wells in the selected area,We found that volcanic rocks were mainly intermediate and basic lava,amygdala develop... |
| |
| Keywords: | volcanic rock laumontite dissolution accumulation of oil and gas |
| 本文献已被 CNKI 万方数据 等数据库收录！ |
| 点击此处可从《沉积学报》浏览原始摘要信息 |
| 点击此处可从《沉积学报》下载免费的PDF全文 |
|
