首页> 外文期刊>Petroleum exploration and development >Formation fluid characteristics and hydrocarbon accumulation in the Dongying sag, Shengli Oilfield
【24h】

Formation fluid characteristics and hydrocarbon accumulation in the Dongying sag, Shengli Oilfield

机译:胜利油田东营凹陷地层流体特征与油气成藏

获取原文
           

摘要

Based on the analysis of geochemical characteristics and distribution of different formation waters, a new origin identification standard was established for the formation water in the Paleogene Shahejie Formation in the Dongying Sag. The migration paths of the connate water expelled from source rocks are similar to those of the hydrocarbons coming from the same rocks, so the geochemical characteristics of the connate water coming from the source rocks can be used as auxiliary indexes to study hydrocarbon migration. Considering fluid pressure and formation water distribution, the Paleogene fluids are divided into three fluid systems: normal-pressure open fluid system, overpressure confined fluid system, and transition fluid system. The differences in hydrocarbon-bearing fluid characteristics, hydrocarbon migration dynamic, hydrocarbon-bearing fluid flow type between these fluid systems were studied. According to characteristics of the hydrocarbon-bearing fluid charging into traps, and formation water drainage pattern, three typical oil accumulation models were classified. In the overpressure confined fluid system, the main oil accumulation mode is high oil saturation fluid entering traps and displacing formation water, and “continuous” reservoirs are prone to form, and fluid oil saturation, fluid charging pressure and fluid seeping conditions affect reservoirs’ oil accumulation extent. In the normal-pressure open fluid system, the main oil accumulation modes include low oil saturation fluids enter a trap while formation water is overflowing out of the trap, and low oil saturation fluids enter a trap while formation water is seeping out of the trap. The amount of hydrocarbon-bearing fluid, fluid oil saturation, trap height, and caprock sealing ability affect reservoir's oil accumulation extent.
机译:在分析不同地层水地球化学特征和分布的基础上,建立了东营凹陷古近系沙河街组地层水成因识别的新标准。从烃源岩中排出的原生水的运移路径与从同一岩石中排出的烃类的运移路径相似,因此可以将来自烃源岩的原生水的地球化学特征作为研究烃类运移的辅助指标。考虑到流体压力和地层水分布,古近纪流体分为三个流体系统:常压开放流体系统,超压受限流体系统和过渡流体系统。研究了这些流体系统之间的含烃流体特性,烃运移动力学,含烃流体流动类型的差异。根据圈闭中含烃流体的特征和地层水的排泄规律,对三种典型的油藏模型进行了分类。在超压密闭流体系统中,主要的油藏模式是高含油饱和度的流体进入圈闭并驱替地层水,并且容易形成“连续”储层,并且流体的含油饱和度,流体充注压力和流体渗漏条件会影响储层的油。积累程度。在常压开放式流体系统中,主要的油藏模式包括低油饱和度的流体进入一个捕集器,同时地层水溢出该阱,而低油饱和度的流体进入一个捕集器,同时地层水从阱中渗出。含烃流体的数量,流体的油饱和度,圈闭高度和盖层的封闭能力都会影响油藏的成藏程度。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号