ISSN 1004-4140
CN 11-3017/P
白清云, 杨威, 马时刚. 一种基于二元回归的时深转换新方法[J]. CT理论与应用研究, 2015, 24(2): 191-197. DOI: 10.15953/j.1004-4140.2015.24.02.05
引用本文: 白清云, 杨威, 马时刚. 一种基于二元回归的时深转换新方法[J]. CT理论与应用研究, 2015, 24(2): 191-197. DOI: 10.15953/j.1004-4140.2015.24.02.05
BAI Qing-yun, YANG Wei, MA Shi-gang. A New Method Based on Binary Regression for Time-depth Conversion[J]. CT Theory and Applications, 2015, 24(2): 191-197. DOI: 10.15953/j.1004-4140.2015.24.02.05
Citation: BAI Qing-yun, YANG Wei, MA Shi-gang. A New Method Based on Binary Regression for Time-depth Conversion[J]. CT Theory and Applications, 2015, 24(2): 191-197. DOI: 10.15953/j.1004-4140.2015.24.02.05

一种基于二元回归的时深转换新方法

A New Method Based on Binary Regression for Time-depth Conversion

  • 摘要: 南堡凹陷C油田沙河街组发育一套披覆在潜山之上的生屑云岩储层,为该油田的主力含油层系,生屑云岩分布不稳定,横向变化较大,先期钻探的5口探井有2口落空。基于周边油田分析,古地貌是生屑云岩储层分布的主要因素。受上覆火成岩的影响,该油藏速度横向变化剧烈,古地貌恢复困难,使预测储层分布范围困难较大。考虑到速度横向变化的影响,利用传统的时深转换方法难以准确地计算构造深度进而恢复古地貌。本文从多口已钻井的时深关系精细对比分析出发,明确了该区的速度影响因素主要有压实效应和火成岩厚度,同时基于对传统时深转换方法的适用性分析,提出了一种基于二元回归的时深转换新方法。实际资料应用表明,利用该方法计算的构造深度与实钻结果吻合较好,能够有效恢复古地貌和预测生屑云岩的分布,该时深转换方法对于速度横向变化剧烈的地区有较好的推广应用价值。

     

    Abstract: A set of buried-hill draping bioclastic dolostone developed in Shahejie Formation in C oilfield of Nanpu depression, Because of the effects of regional geological background, it generally has the following characteristics which create more difficulties in highly efficient development of horizontal wells, such as: complicated reservoir structures, strong lateral velocity variation. As the velocity is of strong lateral variation, it is difficult to accurately calculate the reservoir's structure with traditional method for time-depth conversion. According to the detailed study of time-depth relationship in boreholes, compaction effect and thickness of volcanic rock are confirmed as the two factors affecting the velocity. Based on analysis of traditional method for time-depth conversion. An integrated workflow has been established in this study to improve the prediction accuracy of reservoir depth. According to the detailed study of time-depth relationship in drilled boreholes, compaction effect and thickness of high-speed volcanic rock are confirmed as the two factors affecting the velocity, so we focus on the distribution of the two factors. Initial processing in the time domain was designed to attenuate noise and enhance the signal in the data. This improvement has made it possible to interpret and map above-mentioned two factors in seismic. Elaborate interpretation can depict the reflection time of Ordovician strata which can represent the factor of compaction effect. There existed complex types of volcanic rocks, including volcanic lava and pyroclastic rocks in the area. Based on the mechanism of volcanic eruption and the seismic data, a fact is attained that only the high-speed pyroclastic rocks, namely the effective volcanic rock, account for the lateral velocity variation, from which the relationship between interval velocity of volcanic layer and thickness ofpyroclastic rock is established innovatively to define the second velocity influence factor. On the premise of above effort, which helps us get the distribution of the two factors, we introduce the binary regression to get the average velocity of the reservoir. The average velocity is regarded as the dependent variable of the binary regression while compaction effect and thickness of effective volcanic rock are regarded as the two independent variables. Through the ultra factor of thickness of effective volcanic rock, the new time-depth conversion approach takes full consideration of the lateral variation of velocity, which makes it more suitable for the time-depth conversion of the volcanic-covered reservoir. Application of the field data shows that the depth calculated from the new method matches the actual drilling results very well, and the calculation results could objectively reflect the structural form of the oil-bearing reservoirs.

     

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