PRE-STACK SEISMIC INVERSION BASED ON A GENETIC ALGORITHM: A CASE FROM THE LLANOS BASIN (COLOMBIA) IN THE ABSENCE OF WELL INFORMATION

E. Moncayo, N. Tchegliakova, Luis Montes
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引用次数: 7

Abstract

The Llanos basin is the most prolific of the Colombian basins; however few stratigraphic plays have been explored due to the uncertainty in determining the lithology of the channels. Inside a migrated 2D section, a wide channel was identified inside a prospective sandy unit of the Carbonera Formation, composed by intercalations of sand and shale levels, and considered a main reservoir in this part of the basin. However, the lithology filling the channel was unknown due to the absence of wells. To infer the channel lithology, and diminish the prospective risk a model based pre-stack seismic inversion was proposed. However, without well logs available along the line, the uncertain initial model diminishes reliance on the inversion. To circumvent this impasse, a seismic inversion with a genetic algorithm was proposed. The algorithm was tested on synthetic seismograms and real data from an area of the basin, where well logs were available. The error analysis between the expected and the inverted results, in both scenarios, pointed out a good algorithmic performance. Then, the algorithm was applied to the pre stack data of the 2D line where the channel had been identified. According to the inverted results and rock physics analysis of wells near the seismic line with comparative geology, classified the channel was described as to be filled by silt, shale and probably some levels of shaly sands, increasing the exploratory risk because this lithology has low porosity and permeability, contrary to the producing reservoirs in neighbor fields, characterized by clean sands of high porosity. The algorithm is useful in areas with few or no borehole logs.
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基于遗传算法的叠前地震反演:以哥伦比亚llanos盆地为例
Llanos盆地是哥伦比亚盆地中最多产的盆地;然而,由于河道岩性的不确定性,勘探的地层油气藏很少。在一个迁移的2d剖面中,在石炭纪组的一个远景砂质单元内发现了一条宽阔的河道,由砂层和页岩层的夹层组成,被认为是该盆地的主要储层。然而,由于没有井,填充通道的岩性未知。为了推断通道岩性,降低勘探风险,提出了一种基于叠前地震反演模型的方法。然而,由于没有测井资料,不确定的初始模型减少了对反演的依赖。为了避免这一僵局,提出了一种基于遗传算法的地震反演方法。该算法在盆地某地区的合成地震图和真实数据上进行了测试,该地区有测井数据。在这两种情况下,期望结果与反转结果之间的误差分析指出了良好的算法性能。然后,将该算法应用于已识别信道的二维线叠前数据。根据地震线附近井的反演结果和岩石物理对比分析,将该通道划分为粉砂、页岩,可能还存在一定程度的沙砂,由于该岩性的低孔低渗特点,与邻近油田的高孔净砂生产储层形成对比,增加了勘探风险。该算法适用于测井曲线较少或没有测井曲线的地区。
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