济阳坳陷前第三系顶部风化壳结构发育特征及对油气成藏的影响
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本文为中国石化股份有限公司“济阳坳陷第三系不整合油气藏形成与分布规律”项目(编号P06012)资助的成果。


Structure Characteristics of Weathered Crust at the Top of Pre-Tertiary in the Jiyang Depression and Its Influence on Reservoir Formation
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    摘要:

    基于地质综合研究,系统分析了济阳坳陷前第三系顶部风化壳结构地质特征,深入剖析了其形成主控因素,总结了风化壳结构发育模式,探讨了风化壳结构对油气成藏的影响。研究认为,济阳坳陷前第三系顶部风化壳中,风化粘土层厚度薄,分布地区局限,物性差;半风化岩石全区发育,岩石类型多样,除部分半风化碳酸盐岩、火成岩、变质岩等顶部存在一层致密“硬壳”外,物性多得到改善。风化壳结构形成受控于原岩岩性、间断时间、古气候、古地形、上覆层沉积环境等5大因素;多种因素共同作用,决定了风化壳结构空间发育;风化粘土层、半风化岩石顶部“硬壳”对油气起遮挡、封盖作用,顶部无“硬壳”的半风化岩石则可大大提高前第三系岩层的储集性能和不同层系之间的横向连通性。

    Abstract:

    Based on integrated study, the paper discussed the structural characteristics of the weathered crust on top of Pre-Tertiary in the Jiyang depression. Key factors controlling its formation, structural model of the weathered crust and its influence on the reservoir formation were also discussed. The research showed that weathered clay layer in the studied weathered crust is thin with limited distribution, suggesting a poor reservoir property;while semi-weathered rock of various lithologies extensively developed in the whole area, except for the tight "crust" on the top of semi-weathered carbonate stone, reservoir property was improved obviously. Structure of weathered crust is controlled by lithofacies, paleoclimate, weathering time, paleotopography, and sedimentary environment of the overlying strata. All these factors determine spatial distribution of the structure of weathered crust. The weathered clay layer and "crust" on the top of semi-weathered rock serves as caprock for petroleum reservoir, while semi-weathered rock without “crust” can improve reservoir property of Tertiary system and serve as lateral migration path between different strata.

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赵乐强,张金亮,宋国奇,隋风贵,王学军,向立宏.2009.济阳坳陷前第三系顶部风化壳结构发育特征及对油气成藏的影响[J].地质学报,83(4):570-578.
ZHAO Leqiang, ZHANG Jinliang, SONG Guoqi, SUI Fenggui, WANG Xuejun, XIANG Lihong.2009. Structure Characteristics of Weathered Crust at the Top of Pre-Tertiary in the Jiyang Depression and Its Influence on Reservoir Formation[J]. Acta Geologica Sinica,83(4):570-578.

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  • 收稿日期:2008-03-05
  • 最后修改日期:2008-10-30