利用表层模型的波场延拓基准面校正方案(英文)
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摘要
在复杂近地表条件下采集的地震资料,由于地形起伏剧烈、低降速带变化大,采用传统的铅垂时移静校正方法使地震波场发生扭曲,不利于波动方程偏移成像。本文提出了一种近地表层析反演与波场延拓联合基准面校正的方法,解决复杂近地表条件下采集地震资料的静校正问题。首先是利用折射波层析反演得到近地表模型;其次是炮检点波场延拓。将基准面置于地形之上,根据惠更斯—菲涅尔原理和波场互易原理以及炮检点的空间分布位置,以地表上接收的地震数据为二次震源,将炮检点分别先向下、后向上延拓到地表之上的水平基准面上,从而实现复杂近地表条件下,地震数据层析反演与波场延拓联合基准面校正。
When topography and low velocity zone differences vary greatly, conventional vertical static time shifts will cause wavefield distortion and influence wave equation seismic imaging for seismic data acquired on a complex near surface. In this paper, we propose an approach to datum correction that combines a joint tomography inversion with wavefield continuation to solve the static problem for seismic data on rugged acquisition topography. First, the near surface model is obtained by refracted wave tomography inversion. Second, the wavefield of sources and receivers are continued downward and upward to accomplish datum correction starting from a flat surface and locating the datum above topography. Based on the reciprocal theorem, Huygens’ and Fresnel principles, the location of sources and receivers, and regarding the recorded data on the surface as a secondary emission, the sources and receivers are upward-continued to the datum above topography respectively. Thus, the datum correction using joint tomography inversion and wavefield continuation with the condition of a complex near surface is accomplished.
引文
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