Lithologic Reservoirs ›› 2009, Vol. 21 ›› Issue (1): 11-14.doi: 10.3969/j.issn.1673-8926.2009.01.003
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WANG Yongshi
[1] 徐国盛,李国蓉,王志雄. 济阳坳陷下古生界潜山储集体特征[J].石油与天然气地质,2002,23(3):248-251. [2] 李丕龙,张善文,王永诗,等.多样性潜山成因、成藏与勘探[M].北京:石油工业出版社,2003:44-51. [3] 李丕龙,张善文,王永诗.断陷盆地多样性潜山成因及成藏研究———以济阳坳陷为例[J].石油学报,2004,25(3):28-31. [4] 马立驰,王永诗,姜在兴,等.断陷盆地碳酸盐岩潜山储层模式———以渤海湾盆地济阳坳陷为例[J].石油实验地质,2006,28(1):21-24. [5] 黄思静,石和,张萌.锶同位素地层学在碎屑岩成岩研究中的应用[J].沉积学报,2002,20(3):359-366. [6] 刘昊年,黄思静,胡作维,等.锶同位素在沉积学中的研究与进展[J].岩性油气藏,2007,19(3):59-65. [7] 林会喜. 济阳坳陷桩西—埕岛地区下古生界白云岩储集空间形成机理[J].油气地质与采收率,2006,13(3):5-11. |
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