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Strain energy density distribution of a tight gas sandstone reservoir in a low-amplitude tectonic zone and its effect on gas well productivity: A 3D FEM study

机译:低幅度构造区紧煤砂岩储层的应变能密度分布及其对气体井生产率的影响:3D FEM研究

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The tight gas sandstone reservoirs in the Paleozoic of the Sulige gas field in China are highly heterogeneous, and fractures are key factors for stable reservoir production. Low-amplitude folds or nose-like structures are widely developed in the Upper Paleozoic strata in this area. To effectively predict gas well productivity, in this paper, a 3D FEM numerical simulation based on the deformation and energy variation of the rock mass was used to predict the "sweet spots" of gas well productivity in a tight gas sandstone reservoir using the He8 segment of the Middle Permian Xiashihezi Formation in the Central Sulige block as an example. The paleotectonic stress field of the study area during the maximum episode of compression in the Yanshanian movement was restored, and the two rupture parameters of the integrated rupture rate (IF) and strain energy density (U) were constructed. The strain energy density distribution has a high correlation with gas well productivity, indicating that it can better predict the rock rupture degree in low-amplitude tectonic zones. A complex relationship exists between the strain energy density distribution and low-amplitude folds. The high strain energy density zones are mainly distributed among the high positions and wing areas of the low-amplitude fold zone, but the top area of the low-amplitude fold does not necessarily have a high strain energy density. Portions of the high strain energy density zones are located in the gentle tectonic zone, located near but outside the low-amplitude fold zone. The strain energy in these gentle tectonic zones with a high strain energy density value is relatively high, and the rock mass is prone to rupture. This study is of great value in enriching the prediction of "sweet spots" in tight gas sandstone reservoirs in low-amplitude tectonic zones worldwide.
机译:古生代古生代的古生代砂岩储层是高度异质的,骨折是稳定储层生产的关键因素。低幅度折叠或鼻子状结构在该区域的上古生代地层中广泛开发。为了有效地预测气体良好的生产率,本文采用了一种基于岩石质量变形和能量变化的3D对数值模拟来预测使用HE8段,预测储气砂岩储层中气井生产率的“甜点”中部二叠纪XIASHHIHEZI在中央苏里格砌块中形成的例子。恢复了燕山运动中压缩最大集中的研究区域的古莲应力场,构建了综合破裂率(IF)和应变能密度(U)的两个破裂参数。应变能密度分布与气体井生产率具有高的相关性,表明它可以更好地预测低幅度构造区域的岩石破裂程度。在应变能密度分布和低幅度折叠之间存在复杂的关系。高应变能密度区域主要分布在低幅度折叠区的高位置和机翼区域中,但低幅度折叠的顶部面积不一定具有高应变能密度。高应变能量密度区域的部分位于温和的构造区域,位于低幅度折叠区附近但外部。具有高应变能密度值的这些温和构造区域中的应变能相对较高,并且岩体容易破裂。本研究具有很大的价值,在全世界低幅度构造区域中的狭窄气砂岩储层预测中丰富了“甜点”。

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