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Development of the rocks fracturing model on the Carpathian region example

机译:喀尔巴阡山区岩石压裂模型的发展

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The proposed model will allow evaluating the fracturing of the sandy seams, taking into account geodynamic processes. The model is based on the fact that the main factor in the formation of the original fracturing is stress-deformation state of the rocks during the period of active geodynamic processes. The mechanical properties of the Carpathian rocks are processed for such estimation. Samples of rocks were selected according to stratigraphy, lithology and depth. Sediments of Cretaceous system, Paleogene and Neogene take part in a geological structure of the territory. Age of rocks, lithology and depth are taken into account when sampling for further research, because these parameters can change the mechanical properties of rocks. The 2D finite element model is developed, that model will demonstrate the dependence of fracture strength on the geometric characteristics of a sandstone seam within the anticline. The results of these studies will make it possible to be tter predict the high permeability zones for the epigenetic reservoirs formation. This will allow conducting the secondary explorations of the oil and gas fields.
机译:考虑到地球动力学过程,所提出的模型将允许评估砂接缝的压裂。该模型的基础是,在有源地球动力学过程的时期期间,原始压裂形成的主要因素是岩石的应力变形状态。处理喀尔巴阡岩石的机械性能以进行这种估计。根据地层,岩性和深度选择岩石样品。白垩纪系统的沉积物,古烯和新生,参加了该领土的地质结构。当采样进一步研究时,考虑到岩石,岩性和深度的年龄,因为这些参数可以改变岩石的机械性能。开发了2D有限元模型,该模型将展示断裂强度对背斜内砂岩缝的几何特性的依赖性。这些研究的结果将使能够预测表观遗传储层形成的高渗透区。这将允许进行石油和天然气场的二次勘探。

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