首页> 外文会议>Indonesian Petroleum Association of Annual Convention >RELATIONSHIP BETWEEN FRACTURE DISTRIBUTION AND CARBONATE FACIES IN THE RAJAMANDALA LIMESTONE OF WEST JAVA REGION
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RELATIONSHIP BETWEEN FRACTURE DISTRIBUTION AND CARBONATE FACIES IN THE RAJAMANDALA LIMESTONE OF WEST JAVA REGION

机译:西爪哇省西爪哇地区Rajamandala石灰石骨折分布与碳酸盐相之间的关系

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Fractures can act as a major control on porosity distribution in carbonate reservoirs. Fractures in limestone can be found in a wide range of scales, from millimeters to tens of meter long. In general, two different types of open fractures can be found; extensional fractures and stylolites. Both types can be equally important in controlling porosity and permeability distribution. One of the major problems in reservoir simulation of carbonate rocks is to determine the relationship between fracture distribution and facies. Detailed outcrop study of the Oligo-Miocene Rajamandala Formation has been carried out to characterize fracture type, distribution and density. The field observations were made using the one dimensional scan-line method and the data was analyzed utilizing standard statistical methods.
机译:骨折可以作为碳酸盐储层孔隙率分布的主要控制。石灰石中的骨折可以在各种鳞片中找到,从毫米到几十米长。通常,可以找到两种不同类型的开放性裂缝;延长骨折和牙岩。两种类型在控制孔隙率和渗透性分布方面都同样重要。碳酸盐岩石储层模拟中的一个主要问题是确定骨折分布与面部之间的关系。已经进行了详细的露头研究寡核苷酸rajamandala形成,以表征骨折型,分布和密度。使用一维扫描线法进行现场观察,并利用标准统计方法分析数据。

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