盆地建模作为研究区域油气生成过程和油气资源替代可能性的工具——以特雷戈罗德斯科-康达科夫斯科耶油田为例

V. Zubkov, P. Molodykh, I. Goncharov, V. Samoilenko, S. Fadeeva
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引用次数: 0

摘要

本文介绍了为期两年的研究成果,旨在补充托木斯克地区西北部的资源和原材料基础。说明了盆地建模在地下地质研究勘探阶段的实际应用可能性。研究分为两个阶段。其中第一个是分区域覆盖,包括2.5万平方公里的面积,以东南部的Chkalovsky油气凝析油田和西北部的托木斯克州行政边界为界。该部分仅限于亚历山德罗夫斯基拱门,覆盖了科尔托戈尔斯科-纽罗尔斯基滑道的一部分和尼日涅瓦托夫斯基拱门的东部边缘。第一阶段,建立含油气盆地形成的三维模型,其任务是补充生成史和油气运移方式的认识。在此重建了盆地淹没,恢复了热流历史。该地区沉积盖层底部的热流强度不均匀可以用构造过程来解释,并因大量花岗岩类侵入而变得复杂。在“托木斯克石油研究所”,多年来形成了西西伯利亚油气烃源岩和油的地球化学特征知识库,使其能够在调查区域使用自己的动力学谱。利用镜质组煤的光学特征和巴热诺夫组有机质地球化学特征指标(4/1 MDBT和Tmax)对古地温进行了标定。得出了两个不同性质生油中心的存在,并预测了巴济诺夫组有机质生油的时间和体积。其次,介绍了油气运聚的建模参数。模拟结果表明,烃源岩在生烃过程中出现异常高的孔隙压力和流体自破裂导致了首次运移。比较了两种方法的二次偏移计算结果。尽管存在一些局限性,但得到的结果显示出与实际数据有相当高的收敛性。在第二阶段,在区域(母)模型的基础上,绘制了三维地震勘探覆盖面积为480平方公里的Traygorodsko-Kondakovskoye油田地层的局部子模型。在开始建立详细的局部阶段模型之前,对流体和油源岩进行额外的特殊地球化学研究的必要性和结果的描述给出了理由。本文概述了基本参数,并给出了本地模型和父模型之间的区别。得出了在矿床形成过程中评价断层导电性的可能性。圈闭饱和度预测和资源潜力评价是研究成果,其成果降低了地质勘探风险,为进一步开展地下地质研究提供了建议。
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Basin Modeling as a Tool for Research of Regional Oil and Gas Generation Processes and the Possibility of Replacement of Oil and Gas Riches Illustrated through Traygorodsko-Kondakovskoye Oil Field
The article presents the results of two-year of research aimed at replenishing the resource and raw material base of the northwestern part of the Tomsk region. The practical application possibilities of basin modeling at the prospecting and exploratory stages of geological study of the subsurface are illustrated. The research was divided into two phases. The first of them has sub-regional coverage and includes an area of 25,000 km2 bounded by the Chkalovsky oil and gas condensate field in the southeast and the administrative boundaries of Tomsk Oblast in the northwest. The section is confined to the Alexandrovsky arch, covers part of the Koltogorsko-Nyurolsky chute and the eastern periclinal of the Nizhnevartovsky arch. At the first stage, a three-dimensional model of oil-and-gas bearing basin formation was created, the tasks of which were to replenish the history of generation and formation of ideas about the ways of hydrocarbon migration. The basin submergence has been reconstructed here and the thermal flow history has been restored. The uneven intensity of heat flow at the bottom of the sedimentary cover over the area is explained by tectonic processes and is complicated by a massive granitoid intrusion. In JSC "Tomsk Petroleum institute", the knowledge base of geochemical features of oil-and-gas source rocks and oils of Western Siberia was formed for years, which allowed to use their own kinetic spectra for the surveyed region. To calibrate the paleotemperatures, both the optical characteristics of vitrinite coals and the indicators of the geochemical properties of organic matter of the Bazhenov formation (4/1 MDBT and Tmax) were used. As a result, the conclusion about the presence of two generation centers of different nature was made, the time and volume of oil generation by organic matter of the Bazhenov formation were predicted. Next, the modeling parameters of hydrocarbon migration and accumulation are described. Modeling shows that the primary migration occurs due to the emergence of abnormally high pore pressure during the generation of hydrocarbons and fluid autofracture of the oil and gas source rock. The results of calculations of secondary migration by two different methods are compared. Despite a number of limitations, the results obtained show a fairly high convergence to real data. At the second stage, on the basis of the regional (parent) model a local daughter model of the formation of the Traygorodsko-Kondakovskoye field within the area of 480 km2 covered by 3D seismic exploration was plotted. The rationale for the necessity and description of the results of additional special geochemical studies of fluids and oil source rock, carried out before starting to build a detailed model of the local stage, is given. The article outlines the basic parameters and gives the differences between the local model and the parent model. Conclusions are made about the possibility of assessing the conductive properties of fault in the formation of deposits. The prediction of trap saturation and resource potential assessment is the result, the achievement of which reduced the risks of geological exploration and formed the recommendations for further geological study of the subsurface.
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