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Interdependence of Petrophysical Properties and Depth: Some Implications of Multivariate Solution on Distinction Between the Lower Pontian Hydrocarbon-bearing Sandstone Units in the Western Part of the Sava Depression

机译:岩石物理性质和深度的相互依存:多元溶液对萨瓦Western陷西部下部笨珍烃类下砂岩单元区分的一些影响

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摘要

Statistical analysis of reservoir data from the Lower Pontian clastics (the most important hydrocarbon reservoir rocks in the Sava depression), supports established knowledge of the interdependence of petrophysical properties and depth. Irrespective of the focus that the reservoir data may be studied and presented, depth always emerges as a fundamental reservoir descriptor. This is particularly evident when studying the differences between widely spaced oil and gas fields, when the numerical model completely separates the two sets of descriptor variables, indicating two different sources of their internal variability. Porosity and permeability belong to “intrinsic rock properties” while depth must be ascribed to other sources, e.g. tectonic subsidence. Discriminant function weighted with depth (DF1) has such group centroid values, that zones can be drawn within a particular field that coincide with structural relationships. On the function marked with reservoir properties (DF2), group centroid values are higher close to the axes of palaeotransport channels, where sandstone layers are the thickest and particles are best sorted. Group centroid values on the third function (DF3) depict the areas of relatively higher permeability in the apical parts of structures, possibly caused by fracturing due to folding, or by cementation of other parts of reservoirs, where the circulation of pore waters was more pronounced. In the case of the most thoroughly investigated Zutica field, the inverse relationship between depth and porosity becomes evident when compared with the direction of palaeotransport and thickness of reservoir rocks on the respective structure and thickness maps.
机译:来自下庞统碎屑岩(萨瓦凹陷中最重要的烃类储集岩)的储层数据的统计分析,支持了有关岩石物性和深度相互依存关系的公认知识。不管可以研究和提供储层数据的重点是什么,深度总是作为基本的储层描述符出现的。当研究广泛分布的油气田之间的差异时,当数值模型将两组描述变量完全分开时,这表明内部差异的两个不同来源时,这一点尤为明显。孔隙度和渗透率属于“固有岩石性质”,而深度必须归因于其他来源,例如构造沉降。以深度(DF1)加权的判别函数具有这样的组质心值,即可以在与结构关系一致的特定字段内绘制区域。在标有储层特性(DF2)的函数上,组质心值靠近古输送通道的轴较高,在该通道中,砂岩层最厚,而颗粒则得到最佳分类。第三个函数(DF3)上的组质心值描述了结构顶部的渗透率相对较高的区域,这可能是由于折叠引起的裂缝或储层其他部分的胶结引起的,孔隙水的循环更为明显。在最深入研究的祖蒂卡油田的情况下,与古构造的传输方向和储层岩石厚度在相应的结构和厚度图上相比,深度与孔隙度之间的反比关系变得明显。

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