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首页> 外文期刊>Journal of Zhejiang University Science: An international applied physics & engineering journal >The fracture network model of Shen 229 block buried hill: A case study from Liaohe Basin, China
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The fracture network model of Shen 229 block buried hill: A case study from Liaohe Basin, China

机译:沉229块潜山裂缝网络模型-以辽河盆地为例

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High oil production from the Proterozoic formation of Shen 229 block in Damingtun Depression, Liaohe Basin, China, indicates the presence of natural fractured reservoir whose production potential is dominated by the structural fracture. A consistent structural model and good knowledge of the fracture systems are therefore of key importance in reducing risk in the development strategies. So data from cores and image logs have been collected to account for the basic characteristics of fracture, and then the analyzed results were integrated with the structural model in order to restrict the fracture network development during the structural evolvement. The structural evolution of the Proterozoic reservoir with time forms the basis for understanding the development of the 3D fracture system. Seismic interpretation and formation correlation were used to build a 3D geological model. The fault blocks that compose the Proterozoic formation reservoir were subsequently restored to their pre-deformation. From here, the structures were kinematically modeled to simulate the structural evolution of the reservoirs. At each time step, the dilatational and cumulative strain was calculated throughout the modelling history. The total strain which records the total spatial variation in the reservoir due to its structural history, together with core data, well data and the lithology distribution, was used to simulate geologically realistic discrete fracture networks. The benefit of this technique over traditional curvature analysis is that the structural evolution is taken into account, a factor that mostly dominates fracture formation.
机译:中国辽河盆地大明屯凹陷沉229区块元古生界地层高产,表明存在天然裂缝性储层,其生产潜力以结构性裂缝为主。因此,一致的结构模型和对裂缝系统的充分了解对于降低开发策略中的风险至关重要。因此,从岩心和图像测井中收集数据来解释裂缝的基本特征,然后将分析结果与结构模型整合起来,以限制结构演化过程中裂缝网络的发展。随着时间的推移,元古代储层的结构演化构成了了解3D裂缝系统发育的基础。使用地震解释和地层相关性来建立3D地质模型。组成元古代地层储层的断层块随后被恢复到其变形前状态。从这里开始,对结构进行运动学建模,以模拟储层的结构演化。在每个时间步长,在整个建模历史中计算膨胀应变和累积应变。记录因储层结构历史而引起的储层总空间变化的总应变,连同岩心数据,井数据和岩性分布一起,用于模拟地质上真实的离散裂缝网络。与传统曲率分析相比,该技术的优势在于考虑了结构演化,这是一个主要影响裂缝形成的因素。

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