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Will it or won't it flow!! - A Novel Approach to Understand and Characterize the Fractures for Fluid Conductivity in Basement Reservoirs

机译:它会或不会流动! - 一种理解和表征地下室储层流体电导率骨折的新方法

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Madanam field in Cauvery basin in the east coast of India, has fractured gneissic basement. As exploration focus moved to unconventional reservoirs, the gneissic basement of Madanam was seen as a potential reservoir. However, ambiguity existed about the fluid flow through the basement. For example, in Madanam field, one well (well A) flowed whereas another well (well B) located 8.5 km away had minor flow from the basement reservoir that lasted 2 days. The main purpose of this study was to find possible reasons for this anomalous behavior. This study was conducted by integrating sonic and image measurements with a geomechanics workflow to identify critically stressed open fractures. Further, this work aims to provide a fit-for-purpose solution to optimize and prioritize testing zone selection in near real time.
机译:Madanam领域在印度东海岸的Cauvery盆地,已骨折神道地下室。随着勘探重点迁移到非传统水库,Madanam的神奇地下室被视为潜在的水库。然而,关于流体流过地下室的歧义存在歧义。例如,在Madanam领域,一个井(a)流动,而另一个井(B)位于8.5公里的地面,从持续2天的地下室水库的微小流动。本研究的主要目的是找到这种异常行为的可能原因。通过将声波和图像测量与地质力学工作流程集成来进行该研究,以识别批判性强调的开放性裂缝。此外,这项工作旨在提供适合的解决方案,以优化和优先考虑在近实时选择的测试区选择。

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