Hydrocarbon origin and distribution regularity in Fulin sub-Sag, Zhanhua Sag, Bohai Bay Basin
-
摘要: 通过对渤海湾盆地沾化凹陷富林洼陷原油的生物标志物分布与组合特征分析,认为该区主要存在3类原油:Ⅰ类原油主要分布于东次洼,呈植烷优势,伽马蜡烷含量高,重排甾烷与4-甲基甾烷含量较低,来源于东次洼本身的沙四上亚段烃源岩;Ⅱ类原油分布于中次洼洼陷内部,具有姥鲛烷优势、伽马蜡烷含量低、重排甾烷含量高的特征,纵向上不同储层油气来源存在差异,其中浅部储层油气来源于孤南洼陷沙三下亚段烃源岩,深部储层油气主要来自于富林洼陷沙三下亚段烃源岩;Ⅲ类原油分布于中次洼断裂带附近,成熟度较低,姥鲛烷优势,伽马蜡烷含量中等,C28甾烷含量丰富,孕甾烷和重排甾烷含量较低,为孤南洼陷沙一段与富林洼陷沙三下亚段烃源岩所形成的混源油。Abstract: Based on the studies of biomarker distribution and composition of crude oils in the Fulin sub-Sag of the Zhanhua Sag of the Bohai Bay Basin, there are 3 types of crude oil in the study area. The crude oils of type Ⅰ mainly exist in the east of the sub-sag, characterized by low Pr/Ph ratio, high gammacerence content as well as low diasterane and 4-methyl-sterane contents. They are originated from source rocks in the upper subsection of the 4th member of the Shahejie Formation in the east of the sub-sag. The crude oils of type Ⅱ mainly locate in the center of the sub-sag, featured by high Pr/Ph ratio, low gammacerence content and high diasterane content. The origin for oil and gas is different vertically. Hydrocarbon in the middle and shallow reservoirs is mainly originated from source rocks in the lower subsection of the 3rd member of the Shahejie Formation in the Gunan sub-Sag while hydrocarbon in the deep reservoir is mainly originated from source rocks in the lower subsection of the 3rd member of the Shahejie Formation in the Fulin sub-Sag. The crude oils of type Ⅲ mainly distribute around fault belts in the central sub-sag, featured by low maturity, high Pr/Ph ratio, medium gammacerence content, high C28 sterane content as well as low pregnane and diasterane contents, which show mixed-oil characteristics of source rocks from both the 1st member of the Shahejie Formation in the Gunan sub-Sag and the lower subsection of the 3rd member of the Shahejie Formation in the Fulin sub-Sag.
-
Key words:
- biomarkers /
- hydrocarbon origin /
- distribution regularity /
- Fulin sub-Sag /
- Zhanhua Sag /
- Bohai Bay Basin
-
[1] 乐大发,侯帅军.济阳坳陷沾化凹陷富林洼陷成藏条件[J].石油与天然气地质,2008,29(4):433-443. [2] 李胜利,于兴河,陈建阳,等.沾化凹陷Ro分布规律影响有机质成熟度的因素[J].地质力学学报,2005,11(1):90-96. [3] 朱之锦,宋志强,郭学民,等.富林洼陷油气成藏条件与分布规律研究[J].西南石油学院学报,2002,24(5):7-10. [4] 褚庆忠,张树林.渤海湾盆地垦利断裂带构造与油气关系研究[J].地球学报,2004,25(1):73-78. [5] 王秉海,钱凯.胜利油区地质研究与勘探实践[M].东营:石油大学出版社,1992:133-134. [6] 方旭庆,蒋有录,石砥石.济阳坳陷沾化地区断裂特征及其与成藏要素和油气分布的关系[J].油气地质与采收率,2012,19(2):1-4. [7] 高树新,任怀强,杨少春.渤海湾盆地济阳坳陷陈家庄凸起东段北斜坡油源特征及成藏分析[J].石油实验地质,2007,29(1):68-73. [8] 褚庆忠.渤海湾盆地垦利断裂带油气成藏模式[J].新疆石油地质,2010,31(3):232-234. [9] 褚庆忠,张雪勇,王长江.断裂构造与油气运聚关系研究:以沾化凹陷垦利断裂带为例[J].河南石油,2003,17(1):9-14. [10] 张林晔,张春荣.低熟油生成机理及成油体系[M].北京:地质出版社,1999:93-110. [11] 王志杰.高青—平方王潜山带原油地化特征及油源分析[J].断块油气田,2012,19(3):289-293. [12] 袁东山,张枝焕,曾艳涛,等.沾化凹陷渤南洼陷沙四段烃源岩有机相[J].天然气地球科学,2006,17(1):125-132. [13] 杜振川,刘红梅,魏魁生.孤南富林洼陷层序分析与盆地演化[J].河北建筑科技学院学报,2001,18(1):66-68. [14] 朱之锦,姜晓健,廖林.富林洼陷油气运移研究[J].油气地质与采收率,2004,11(1):28-30. [15] 朱光有,金强,丁浩,等.济阳坳陷沾化断陷湖盆沙河街组生烃系统特征[J].天然气工业,2004,23(增刊):10-12. [16] 王乐闻,刘四兵,王鹏,等.沾化凹陷烃源岩地球化学特征分析[J].重庆科技学院学报:自然科学版,2011,13(6):26-28. [17] 李胜利,于兴河,陈建阳,等.渤海湾盆地济阳坳陷沾化凹陷地层流体压力分布规律及其对油气成藏的影响[J].地质力学学报,2006,12(1):37-42.
计量
- 文章访问数: 1785
- HTML全文浏览量: 100
- PDF下载量: 832
- 被引次数: 0