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3D baseline seismics at Ketzin, Germany: The CO2SINK project

机译:德国Ketzin的3D基线地震:CO2SINK项目

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A 3D 25-fold seismic survey with a bin size of 12 by 12 m and about 12 km(2) of subsurface coverage was acquired in 2005 near a former natural gas storage site west of Berlin, as part of the five-year EU funded CO2SINK project. Main objectives of the seismic survey were to verify earlier geologic interpretations of structure based on vintage 2D seismic and borehole data and to map, if possible, the reservoir pathways in which the CO2 Will be injected at 650 m depth, as well as providing a baseline for future seismic surveys and planning of drilling operations. The uppermost 1000 m are well imaged and show an anticlinal structure with an east-west striking central graben on its top that extendsdown to the target horizon. About 30 m of throw is seen on the bounding faults. No faults are imaged near the planned drill sites. Remnant gas, cushion and residual gas, is present near the top of the anticline in the depth interval of about 250-400 m and has a clear seismic signature; both higher amplitudes in the reservoir horizons and velocity pulldown are observed. Amplitude mapping of these remnant gas horizons shows that they do not extend as far south as the injection site, which is located on the southern flank of the anticline. Amplitude anomalies, gas chimneys along an east-west striking fault, show that the stored or remnant gas either has been or is presently migrating out of the reservoir formations. Summed amplitude mapping of the planned injection horizon indicates that this lithologically heterogeneous formation may be more porous at the injection site.
机译:2005年,在欧盟资助的五年资助下,在柏林以西的一处天然气储藏地点附近,进行了3​​D 25倍地震调查,其箱尺寸为12 x 12 m,地下覆盖范围约为12 km(2)。 CO2SINK项目。地震勘测的主要目的是基于老式的2D地震和井眼数据验证结构的早期地质解释,并在可能的情况下绘制将在650 m深度注入CO2的储层通道,并提供基线。用于将来的地震勘测和钻井作业计划。最上面的1000 m被很好地成像,并显示出一个倾斜的结构,其顶部有一个东西向撞击的中央抓斗,向下延伸到目标地平线。在边界断层处可以看到约30 m的投掷。在计划的钻探地点附近没有任何故障成像。背斜顶部附近约250-400 m的深度范围内存在残余气体,垫层和残余气体,并具有清晰的地震特征。观察到储层水平较高的振幅和速度下降。这些残留气体层位的振幅图显示,它们没有延伸到南至延伸到背斜南侧的注入点。幅度异常(沿东西走向的断裂带的烟囱)表明,已储存或剩余的气体已经或正在从储层中迁移出来。计划的注入层的总振幅图表明,这种岩性上的非均质地层在注入部位可能更为多孔。

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