Lithologic Reservoirs ›› 2010, Vol. 22 ›› Issue (Z1): 18-21.doi: 10.3969/j.issn.1673-8926.2010.Z1.005
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QU Weiguang
[1] 黄思静,黄培培,王庆东,等.胶结作用在深埋藏砂岩孔隙保存中的意义[J].岩性油气藏,2007,19(3):7-13. [2] 郑浚茂,庞明.碎屑岩储集岩的成岩作用研究[M].北京:中国地质大学出版社,1989. [3] 许建华,张世奇,纪友亮.藏北羌塘盆地中上侏罗统碎屑岩储层成岩演化特征[J].石油大学学报:自然科学版,2001,25(1):4-8. [4] 黄龙,田景春,肖玲,等.鄂尔多斯盆地富县地区长6 砂岩储层特征及评价[J].岩性油气藏,2005,17(4):42-46. [5] 孟玮,钟建华,李勇,等. 东营凹陷北部陡坡带砂砾岩体分布规律[J].特种油气藏,2009,16(5):17-19. [6] 蔡进功,谢忠怀,田芳,等.济阳坳陷深层砂岩成岩作用及孔隙演化[J].石油与天然气地质,2002,23(1):84-88. [7] 王宝言,隋风贵.济阳坳陷断陷湖盆陡坡带砂砾岩体分类及展布[J].特种油气藏,2003,10(3):38-41. [8] 李利,牛强,杜焕福,等.东营凹陷北部陡坡带盐22 地区沙四段砂砾岩体储层微观特征[J].内蒙古石油化工,2008,(19):97-100. |
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