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A 3D Seismic Traveltime Tomography Study of the Shallow Subsurface at the CO2SINK Project Site, Ketzin, Germany

机译:在德国Ketzin的CO2SINK项目现场进行的浅地下3D地震行时层析成像研究

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3D seismic traveltime tomography is tested at the CO2SINK project site, a small scale storage and monitoring project of CO2 injection into a saline aquifer formation near the town of Ketzin, Germany. The main purpose of this study is to obtain additional information on the inhomogeneous near-surface layers above 150 ms where the 3D reflection seismic image is poor. First arrival traveltimes from a subset of the 3D reflection data were used for this study. We use a 3D traveltime tomography technique based on a combination of solving for 3D velocity structure and static corrections in the inversion process. The resulting velocity model shows low velocities of 800-1000 m/s in the cover of the study area. A velocity contrast of approximately 1600 m/s and 2000 m/s at 60-80 m depth represents the boundary between Quaternary deposits and Tertiary sections. Correlation of the tomographic images with a similarity attribute slice at 150 ms (about 150 m depth) indicates that east-west running fault zones observed in the reflection data may extend into the Tertiary sections. This is shallower than what can be mapped from the reflection seismic images.
机译:在CO2SINK项目现场对3D地震行进时层析成像进行了测试,该项目是在德国Ketzin镇附近的一个盐水注入地层中注入CO2的小规模存储和监控项目。这项研究的主要目的是获得3ms反射地震图像较差的150 ms以上非均匀近地表层的信息。这项研究使用了3D反射数据的子集的首次到达旅行时间。我们基于反演过程中3D速度结构的求解和静态校正的结合使用3D行程时间层析成像技术。所得的速度模型在研究区域的覆盖范围内显示出800-1000 m / s的低速度。在60-80 m深度处,大约1600 m / s和2000 m / s的速度反差表示第四纪沉积物和第三纪剖面之间的边界。断层图像与相似属性切片在150毫秒(约150 m深度)处的相关性表明,在反射数据中观察到的东西走向的断裂带可能延伸到第三纪段。这比从反射地震图像可以映射的要浅。

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