首页> 外文会议>Abu Dhabi International Petroleum Exhibition and Conference >Geometry of Porosity Break Plane Associated with Bitumen Zone and Timing of its Generation in an Upper Jurassic Reservoir, Offshore Abu Dhabi, UAE
【24h】

Geometry of Porosity Break Plane Associated with Bitumen Zone and Timing of its Generation in an Upper Jurassic Reservoir, Offshore Abu Dhabi, UAE

机译:与沥青区域相关的孔隙断裂平面的几何与其在上侏罗纪水库中产生的时间,阿布扎比offshore abu dhabi,阿联酋

获取原文

摘要

An Upper Jurassic reservoir in “Field A” is characterized by existence of bitumen (tar mat) zone intersecting sub- layers in the reservoir and porosity deterioration is observed in the bitumen zone and below bitumen zone. It is obvious that porosity deteriorates significantly at top of the bitumen (Porosity Break Plane: PBP) on core materials and open hole log interpretation, in addition, no flow contribution below PBP was confirmed by production logging data due to its tight nature. Therefore, it is very important to define PBP precisely in order to estimate hydrocarbon reserves and optimize future infill well locations. The thickness of porous interval between top of reservoir and PBP indicates thinning toward the flank area and finally pinching-out in the flank area. The PBP and bitumen have been considered that they were possibly formed near paleo-OWC and the present curved shape of PBP can be attributed structural growth of the field after formation of them by deeper salt swelling. PBP is confirmed at crest and flank wells in different stratigraphic position depending on their structural locations. Based on the detailed structural interpretation of the top reservoir using recently acquired 3D seismic data, the relationship between the top reservoir depth structure and PBP identified in the wells became clear. It is helpful for the PBP mapping and understanding of the bitumen distribution. 3D geological model incorporating PBP was constructed based on the above observation and new structure map derived from 3D seismic interpretation. This workflow helps to improve predictive capability on PBP mapping in non-well control. In addition, based on the structural interpretation of overburden horizons on the 3D seismic data and newly interpreted PBP, the history of structural development and timing of PBP generation were estimated. Based on the back stripping of overburden formations, PBP seems to be flatten in the Shilaif age. This paper discusses the reasonability of this timing.
机译:在“田间A”中的上侏罗缎储存器的特征在于存在沥青(焦油)区域的储存器中的子层和孔隙区和沥青区下方的孔隙率劣化。显而易见的是,在核心材料的沥青(孔隙断裂平面:PBP)顶部显着恶化,并且开放孔对数解释,此外,由于其紧迫性,通过生产测井数据确认了低于PBP的流量贡献。因此,精确地定义PBP是非常重要的,以估计碳氢化合物储备并优化未来的填充井位置。储存器顶部和PBP之间的多孔间隔的厚度表明朝向侧面稀疏并且最终在侧面区域夹出。已被认为PBP和沥青在Paleo-OWC附近可能形成它们在古欧径附近,并且通过更深的盐肿胀形成它们后,PBP的本曲线形状可归因于该场的结构生长。根据其结构位置,在冠和侧面处于不同的地层位置确认PBP。基于使用最近获得的3D地震数据的顶层储层的详细结构解释,井上鉴定的顶部储层深度结构与PBP之间的关系变得清晰。 PBP映射和对沥青分布的理解是有帮助的。基于上述源自3D地震解释的上述观察和新的结构图,构建了包含PBP的地质模型。此工作流程有助于提高非良好控制中PBP映射的预测能力。此外,基于3D地震数据和新解释的PBP对覆盖层视野的结构解释,估计了PBP生成的结构发展史和时序。基于背部剥离覆盖层的形成,PBP似乎在Shilaif时代变平。本文讨论了这个时序的合理性。

著录项

相似文献

  • 外文文献
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