地震属性在尼日尔三角洲盆地西部Tomboy油田断层探测和油气直接指示中的应用

K. Ibekwe, Chinazaekpere M. Arukwe, C. V. Ahaneku, E. Onuigbo, Jerry O. Omoareghan, A. Lanisa, V. O. Oguadinma
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摘要

地震属性分析是地震解释等地下资料解释的重要内容,涉及地震地层和构造解释。这种解释常常受到地震分辨率的阻碍,有时,人类无法识别地震的微妙特征。这些因素经常导致地质特征的地震解释不佳。因此,利用尼日尔三角洲西部约56 km2的三维地震数据,在Tomboy油田开展了一项利用地震属性研究构造模式和含油气带的综合方法。地震体经过叠后处理,增强了地震不连续性。首先建立了一个深度导向体,并应用了几个倾角过滤器来增强研究区域的断层。然后,计算倾角导向和断层增强体的曲率和相似度属性。这些计算显示了断层的详细几何形状和微妙的线条带。识别并绘制了F1、F2、F3、F4、F5、F6 6条断层。这些断层的范围从对偶断层到嵴生长断层。F5和F6两条主要生长断裂呈东北向西南倾斜。在主要断层下方出现了一个接近广泛的断层嵴(F4)。在倾斜地震资料中,虽然在顶部断层的南部和中部显示了几条小裂缝,但西南(F4)和生长断层(F6)负责在已确定的闭包内发现油气。利用地震数据的属性增加了对构造特征作图和解释的信心。此外,能量属性被用作直接油气指标(DHI),以可视化研究中的可行区域,从而实现更可靠的解释。在平坦和亮斑区域拍摄时间片。对这些薄片进行谱分解属性分析,显示出主要由区域-次区域生长断裂圈闭的含油气区典型的高振幅反射区。在生地表上计算的地表属性表明,该油田主要受断层控制,断层是油气的圈闭。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Application of Seismic Attributes in Fault Detection and Direct Hydrocarbon Indicator in Tomboy Field, Western-Offshore Niger Delta Basin
Seismic attribute analysis is important in subsurface data interpretation, such as seismic interpretation, which could involve seismic stratigraphic and structural interpretation. This interpretation is often hampered by seismic resolution and, sometimes, human inability to identify a subtle feature on the seismic. These factors have frequently led to the poor seismic interpretation of geologic features. Thus, an integral approach to studying structural patterns and hydrocarbon bearing zones using seismic attributes was carried out on the Tomboy field using 3D seismic data covering approximately 56 km2 of the western belt of the Niger Delta. The seismic volume underwent post-stack processing, which enhanced seismic discontinuities. A deep steering volume was first created, and several dip filters were applied to enhance faults in the study area. After that, curvature and similarity attributes were calculated on the dip-steered and fault-enhanced volume. These calculations show detailed geometry of the faults and zones of subtle lineaments. Six faults (F1, F2, F3, F4, F5 and F6) were identified and mapped. These faults range from antithetic to crest growth faults. Two major growth faults (F5 and F6) were revealed to dip in the northeast to southwest directions. A near-extensive crest fault (F4) appeared beneath the major faults. Although several minor fractures were displayed in the southern and central portions of the crest fault of the dipping seismic data, the southwest (F4) and growth fault, F6, are responsible for holding the hydrocarbon found within the identified closures. Using attributes on the seismic data increased confidence in mapping and interpreting structural features. Furthermore, energy attributes were used as Direct Hydrocarbon Indicators (DHI) to visualize viable areas within the study, which allows a more robust interpretation. Time slices were taken in regions of flat and bright spots. The spectral decomposition attribute was run on these slices to display areas of high amplitude reflection typical of hydrocarbon-bearing regions trapped mainly by regional to sub-regional growth faults. The surface attribute calculated on the generated surface shows that the field is predominantly controlled by faults serving as traps for hydrocarbon. 
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