摘要
湖南地处扬子陆块和华夏古陆过渡区,湘西北地区至雪峰山东南缘基本位于扬子地台,此区域属南方海相页岩气远景区.本文主要选取地质构造条件优越、页岩气特征较为明显的龙马溪组黑色页岩层作为主要研究对象.研究表明,龙马溪组黑色页岩分布面积广、有机碳含量高（TOC平均值为2.0％）、热演化程度高（Ro平均值为2.59％）、低孔低渗（孔隙度平均值为2.3％、渗透率小于0.04× 10-3μ m2）;黑色页岩产出厚度在石门-桑植复向斜至龙山、来凤一带较厚,基本大于30 m.而其整体埋深范围在1000～2000m之间为主,产出较为平缓.总体认为,此套含气页岩有待进一步详细勘探和研究,也是十分有开发潜力的页岩气目标层.优选区集中在石门-桑植复向斜至雪峰山东南缘.
Hunan Province is located in excessive belt between Yangtze and Cathaysia, and the northwestern Hunan to the southeast Xuefeng orogeny locate in Yangtze platform which belongs to the prospects Of shale gas in southern marine. To select the Longrnaxi Formation black shale as the main study object which have a favorable geological conditions and the more obvious features of shale gas. The results shows that the shale is characterized with wide distribution, high organic content （the average of TOC is 2.0%）, high organic thermal evolution degree （the average of Ro is 2.59%）; the low-porosity and low-permeability （the average of porosity is 2.3%, and the av- erage of permeability is less than 0.04 ×10-3 μm2）; the output thickness of black shale in Shimen-Sangzhi synclinorium to Longshan-Laifeng area is above 30 m; depth range is mainly between 1000 - 2000 m, and rock occurrence is relatively fiat. In short, this set of black shale should do further explorate and study. At the same time, it is a very promising shale gas target layer. Preferred areas are concentrated in Shimen-Sangzhi synclinorium to the southern edge of the Xuefeng Mountain.
出处
《华南地质与矿产》
CAS
2014年第3期285-292,共8页
Geology and Mineral Resources of South China
基金
中央地质矿产调查评价专项地勘基金项目(项目编号:201203084)
关键词
页岩气
龙马溪组
热演化程度
扬子地台
Shale Gas
Longmaxi Formation
thermal evolution degree
Yangtze platform
