首页> 外文期刊>Journal of Geoscience, Engineering, Environment and Technology >Characterization of Basement Fracture Reservoir In Field ‘X’, South Sumatera Basin, Based On The Analysis of Core And FMI Log
【24h】

Characterization of Basement Fracture Reservoir In Field ‘X’, South Sumatera Basin, Based On The Analysis of Core And FMI Log

机译:基于岩心和FMI测井资料的分析,南苏门答腊盆地X地区地下储层裂缝储层特征

获取原文
       

摘要

Basement reservoir is a reservoir that is located in the basement rock, comprised of either igneous rock or metamorphic rock that has secondary porosity, resulting in its capability to store oil and gas. The research was conducted at field 'X' that is located at South Sumatra basin and it is a part of Jambi Sub-Basin. The study was focused on discussing hydrocarbon potential in Fields 'X', particularly at the basement metamorphic rock. The study was conducted at two wells in the field. The secondary porosity system of the basement is fracture porosity. Fracture analysis as secondary porosity system was performed on two wells, HA-1 and HA-2, by using FMI log interpretation. Based on the analysis of fracture on HA-1 well, the trend of fracture system is Northeast - Southwest (NE-SW) with a fracture porosity of 1.49%. On a different note, the trend of fracture system on HA-2 wells is East Northeast - West Southwest (ENE-WSW) with a fracture porosity of 0.888%. The effect of rock properties itself has little influence on the number of fractures as opposed to the effect of surrounding tectonic forces. The fractures are controlled by geological structures following Jambi pattern that has an orientation of Northeast - Southwest (NE-SW). Although the fracture porosity is relatively small, it is enough to storing hydrocarbons in economical quantity.
机译:地下储层是位于地下岩石中的一个储层,由火成岩或变质岩组成,具有次生孔隙度,从而具有储油和天然气的能力。该研究是在位于苏门答腊南部盆地的“ X”油田进行的,该油田是占碑盆地的一部分。该研究的重点是讨论油田“ X”中的油气潜力,尤其是在基底变质岩中。该研究是在现场的两口井进行的。地下室的次生孔隙系统是裂缝孔隙。通过使用FMI测井解释,在两个井HA-1和HA-2上进行了作为二级孔隙度系统的裂缝分析。根据HA-1井的裂缝分析,裂缝系统的走向为东北-西南(NE-SW),裂缝孔隙率为1.49%。另一方面,HA-2井的裂缝系统趋势为东北东-西南(ENE-WSW),裂缝孔隙率为0.888%。与周围构造力的影响相反,岩石性质的影响本身对裂缝的数量影响很小。裂缝由遵循Jambi模式的地质结构控制,Jambi模式具有东北-西南(NE-SW)方向。尽管裂缝孔隙率相对较小,但足以存储经济量的碳氢化合物。

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