天然气地球科学 ›› 2019, Vol. 30 ›› Issue (12): 17711781.doi: 10.11764/j.issn.1672-1926.2019.10.014
• 非常规天然气 • 上一篇
王丹丹1,2(),周新桂1,刘丽红1(),李世臻1,张交东1,张文浩1,刘卫彬1,刘旭锋1,曾秋楠1
Dan-dan Wang1,2(),Xin-gui Zhou1,Li-hong Liu1(),Shi-zhen Li1,Jiao-dong Zhang1,Wen-hao Zhang1,Wei-bin Liu1,Xu-feng Liu1,Qiu-nan Zeng1
摘要:
通化盆地下白垩统亨通山组油气显示好,具有良好的常规和非常规油气勘探前景,但目前缺乏系统总结,特别是对亨通山组泥页岩储层特征的认识尚未开展。以通化盆地首次钻遇油气显示的通地1井岩心为研究对象 ,系统开展了X?射线衍射、扫描电镜、液氮吸附等分析测试。研究结果表明:通化盆地亨通山组泥页岩脆性矿物含量为58.2%,石英脆度为35.4%,有利于压裂改造;孔隙类型主要为有机质孔、微裂缝、粒内孔和粒间孔,其中粒内溶蚀孔最为发育,粒间孔次之;泥页岩孔径分布较复杂,主要分布在2~60nm之间,以中孔为主,其次为微孔和大孔;中孔提供了90.87%的孔隙体积和85.74%的比表面积,是页岩气赋存的主要载体。对影响亨通山组泥页岩孔隙结构的因素进行了探讨,认为有机质丰度和显微组分对该地区孔隙的影响较为明显。
中图分类号:
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