Creation of Geological 3D-Model of Komyshnianske Field Based on the Sequence Stratigraphy Principles

O. Noskov, Serhii Mykhailovych Levoniuk, M. Myrontsov
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Abstract

Currently, the sequence-stratigraphic section dismemberment is only being implemented in Ukraine, so this article is highly relevant. The authors created geological 3D model of Komyshnianske gas condensate field based on sequence-stratigraphic section dismemberment for the first time at this area. This approach is effective for the following conditions:-insufficient field geological study;-thickness of productive horizons does not reach the seismic resolution boundaries;-no significant difference in impedance values on reflection horizons. The selected technique includes the following stages:-field geological study, facies analysis (integration of well geophysical complexes, cores);-deduction and correlation of sequence boundaries;-construction of discrete log, which corresponds to specific sequences distribution;-conducting seismic interpretation of the 3D seismic survey study of research area;-construction of a structural framework with the involvement of correlated sequences boundaries;-comparison of volume seismic attributes with selected sequences distribution. A geological 3D model of Komyshnianske gas condensate field was created based on sequence-stratigraphic principles. During the research, a geological structure of field was analyzed, the separated conditions of sedimentation (sequences) were deducted and interpreted. During the seismic interpretation of 3D seismic survey of study area, local features of wave field were identified, their reflection in the core material was found and linked to the concept of changing sedimentation conditions. With a general understanding of the material transportation and accommodation direction, used method allows to qualitatively outline the distribution boundaries of sedimentation certain conditions and predict their development outside the study area. Construction of facies discrete log and their distribution in the seismic field allows grouping thin bed layers of collectors to reach the seismic resolution and use them to predict the distribution of facies associated with changes in the rocks reservoir properties (tracking beach facies of deltas/avandeltas, sloping sediments, etc.). The constructed model could be used as a trend for reservoir distribution at the stage of construction of static geological model. Involvement of sequence-stratigraphy technique is new approach to sedimentation conditions study within Dnipro-Donetsk depression (DDD) areas. The paper shows that provided methodology gives:-improved geological understanding of field through sedimentation analysis and facies logging;-trends for reservoir properties distribution with the involvement of construction facies volumes;-proposals for further field E&D. The general provisions under conditions of geological materials sufficient base can be applied to other DDD areas, especially in pre-border zones. Involvement of sequence-stratigraphy technique is new approach for sedimentation conditions study within Dnipro-Donetsk depression (DDD) area. On the example of Komyshnianske gas condensate field, the article shows that provided methodology gives:-improved geological understanding of field through sedimentation analysis and facies logging;-trends for reservoir properties propagation with the involvement of seismic volume studies;-propositions for further field Exploration & Development.
基于层序地层学原理的Komyshnianske油田三维地质模型建立
目前,层序地层剖面剖分仅在乌克兰进行,因此本文具有较强的现实意义。在该地区首次建立了基于层序-地层剖面剖分的Komyshnianske凝析气田三维地质模型。该方法适用于野外地质研究不充分、生产层厚度未达到地震分辨率边界、反射层阻抗值差异不明显等情况。所选择的技术包括以下几个阶段:现场地质研究、相分析(井地球物理复合体、岩心的整合)、层序边界的推断和对比、离散测井的构建、—对研究区三维地震调查研究进行地震解释;—构建涉及相关层序边界的构造框架;—将体地震属性与选定的层序分布进行比较。基于层序地层学原理,建立了科米什尼扬斯克凝析气田三维地质模型。在研究过程中,对某油田的地质构造进行了分析,推导并解释了沉积(层序)分离条件。在研究区三维地震调查的地震解释中,识别了波场的局部特征,发现了它们在岩心物质中的反射,并将其与沉积条件变化的概念联系起来。通过对物质运移和容纳方向的大致了解,所采用的方法可以定性地勾勒出一定条件下沉积的分布边界,并预测其在研究区外的发展。相离散测井的构建及其在地震场中的分布,可以将薄层收集器分组,达到地震分辨率,并利用它们来预测与岩石储层物性变化相关的相分布(跟踪三角洲/ avanddelta的滩相、倾斜沉积物等)。所建立的模型可作为静态地质模型构建阶段的储层分布趋势。层序地层学技术的介入是研究第聂伯-顿涅茨克凹陷沉积条件的新途径。本文表明,该方法通过沉积分析和相测井提高了对油田的地质认识;通过建设相量的参与,确定了储层物性分布的趋势;为进一步的油田勘探开发提出了建议。地质物质基础充足条件下的一般规定也可适用于其他DDD地区,特别是边界前地区。层序地层学技术的介入是研究第聂伯-顿涅茨克凹陷沉积条件的新途径。以Komyshnianske凝析气田为例,通过沉积分析和相测井,提高了对气田的地质认识;通过地震体研究,确定了储层物性扩展的趋势;提出了进一步勘探开发的建议。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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