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Practical Application of CFP Technology to Resolve Complex Near Surface Problems and to Estimate a Velocity-depth Model

机译:CFP技术解决复杂近地表问题的实际应用,估算速度深度模型

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Complex topography and highly variable weathering layers in the near surface can severely degrade the quality of seismic data and result in a distorted structural image of the subsurface reflectors. One objective of this work is to compare seismic image quality after application of Common Focus Point (CFP) redatuming with images generated using more conventional statics techniques. The CFP process is independent of any velocity model and derives data-driven focusing operators. CFP operators inherit the kinematic phenomena of the wavefield that passes through the near surface. These operators are estimated using parametric inversion. Using these operators, a complete wavefield redatuming can be performed moving the data recorded at the surface to a new datum underneath the complex near surface. A second objective of this work is to demonstrate that CFP operators can be used in a tomographic inversion process to obtain a fine-tuned velocity-depth model that is more geological in appearance and to determine the actual positions of the focusing points. The redatuming results showed significant improvements over results from traditional statics correction methods in terms of better continuity of the deeper reflection events as well as reliability of the structural time image.
机译:在近表面中的复杂地形和高度可变的风化层可以严重降低地震数据的质量,并导致地下反射器的扭曲结构图像。这项工作的一个目的是在使用使用更多传统估计技术产生的图像中施加共同焦点(CFP)之后比较地震图像质量。 CFP过程与任何速度模型无关,并导出数据驱动的聚焦操作员。 CFP运算符继承穿过近曲面的波场的运动学现象。使用参数反转估计这些运营商。使用这些运算符,可以执行完整的波场重新定义,将记录在表面上的数据移动到近表面上的复杂下面的新基准。这项工作的第二个目的是证明CFP运营商可以用于断层反转过程,以获得微调速度深度模型,该模型在外观上更加地质,并确定聚焦点的实际位置。在更好的反射事件的更好的反射事件以及结构时间图像的可靠性方面,重新定位结果表明,传统静计校正方法的结果显着改善。

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