Elaboration of criteria for laying wells of the operating stock of the Riphean carbonate reservoir in the central part of the Kamovsky arch of the Baikit anteclise based on 3D seismic data

S. S. Soshnikov, E. Cherepanov
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Abstract

Summary The object of this work was a large oil and gas condensate carbonate field in Eastern Siberia. The target interval at the field is the riphean reservoirs, which are represented by an impermeable carbonate matrix permeated by a dense network of micro-macro cracks of various orientations, caverns and leaching intervals. The affected area was subjected to an active and multi-stage tectonic impact, which led to the widespread development of numerous low-amplitude, sub-vertical faults and fracture zones of a predominantly shear nature. The main intervals of the section are represented by the Archean basement, Proterozoic (Riphean-Vend), Paleozoic (Cambrian, Ordovician, etc.) and Upper (HCR) parts of the section. The Paleozoic part of the section consists mainly of Cambrian carbonate-halogen-sulfate rocks and traps, presumably of Triassic age. The wave pattern of the Cambrian rocks is characterized by relatively laterally sustained seismic reflections with a small number of interpreted faults. The shape of the wave pattern, or in other words, the seismic images/seismophations, are mainly high-amplitude, laterally sustained with increased reflection and impedance coefficients. Potential reservoirs in this part of the section are most often represented by relatively dense carbonates, which are characterized by a small number of secondary changes in carbonate rocks. The main risks when drilling GS are the presence of abnormally high absorption of drilling fluid (up to loss of circulation), the presence of tool failures, frequent wear of bits, the presence of silicification. More than half of the current fund of producing wells have a high gas factor or significant water cut. To solve the described problems, it was decided to create a number of criteria for laying horizontal wells, taking into account the seismogeological conditions of the section.
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基于三维地震资料,制定了Baikit前盘Kamovsky拱中部Riphean碳酸盐岩储层作业储层的钻井标准
本文以东西伯利亚某大型凝析碳酸盐岩油气田为研究对象。该油田的目标层段为里芬储层,以不渗透碳酸盐基质为代表,渗透着密集的各种定向、洞室和浸出层段的微宏观裂缝网络。受影响地区受到活跃的多期构造冲击,导致大量低振幅、次垂直断裂和以剪切为主的断裂带广泛发育。剖面的主要层段为太古宙基底、元古代(Riphean-Vend)、古生代(寒武纪、奥陶纪等)和上段(HCR)。该剖面古生代主要由寒武纪碳酸盐岩-卤素硫酸盐岩和圈闭组成,推测为三叠纪。寒武系岩石波型的特征是相对横向持续的地震反射和少量的解释断裂。波型的形状,或者换句话说,地震图像/地震活动,主要是高振幅,横向持续,反射系数和阻抗系数增加。该剖面的潜在储层多为致密碳酸盐岩,其特征是碳酸盐岩发生少量次生变化。GS钻井的主要风险是钻井液吸收率异常高(直至循环损失)、工具故障、钻头频繁磨损和硅化现象。目前超过一半的生产井具有高含气系数或显著含水率。为了解决上述问题,考虑到该剖面的地震地质条件,决定制定一系列水平井的铺设标准。
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