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For imaging the complex subsurface such as salt dome, faults, and folds, we perform prestack migration with surface seismic data or sometimes VSP (Vertical Seismic Profiling) data. The VSP data includes wavefield that can measure directly physical properites between surface and geological interfaces. The VSP is used for detecting dip, anisotropy, and reflection amplitude or waveform with respect to incidence angles. Here we applied forward modeling and prestack migration which are used for surface seismic data to VSP. We made synthetic VSP seismic data using the 8th order finite difference method for the acoustic wave equation and did VSP prestack migration. The synthetic VSP data to a simple three horizontally layered geological model showed the direct waves, reflection and refraction, which includes down-going and up-going waves with different direction. These were similar to the typical VSP data. Usually VSP prestack time migration needs filtering in order to separate up-going and down-going wave, but we did VSP prestack depth migration using inner product of back-propargated wavefield and the virtual source without filtering. The back-propagated wavefield was calculated from observed data and the virtual source was from the forward modeling using the observed data as a source term. The result of numerical modeling for the salt flank model shows that the upper horizontal and dipping layer were properly imaged. The better image of upper horizon and dipping layers than the lower layers indicates that seismic energy was concentrated on this part.
암염돔, 단층, 습곡 등 복잡한 층서구조를 영상화하기 위해서는 지표면 탄성파 자료에 대해 선 중합 깊이영역 구조보정(prestack depth migration)이 필요하며 또한 탄성파 수직탐사(VSP)를 이용하기도 한다. 탄성파 수직탐사는 지표면과 지층경계면 사이에서 직접 물성을 측정할 수 있는 파동장을 기록하는 방법으로 지층경사, 이방성, 입사각에 따른 반사계수 변화, 파형변화 등 파악하는데 적용된다. 여기에서는 지표면 탄성파 자료에 적용되는 모델링과 구조보정법을 VSP자료에 적용하는 연구를 수행하였다. 인공합성 VSP 모델링에는 8차 근사 파동방정식의 유한차분법을 이용하였고, 지층구조 영상화는 가상음원과 역전파 파동장의 내적을 이용하여 실시하였다. 단순 수평 3층 모델에 대한 VSP 인공합성자료를 살펴 볼 때 직접파, 굴절파, 반사파 등이 모두 포함되어 있고 하향파, 상향파가 서로 반대 경사를 가지면서 나타나는 전형적인 VSP 자료 특성을 보여주고 있어 모델링방법이 적절하였음을 확인하였다. VSP 선 중합 깊이영역 구조보정은 상향파와 하향파를 분리하는 전 처리 과정없이 역전파 시킨 관측자료와 관측자료를 음원으로 이용하여 구한 가상음원과의 내적으로 영상을 구하였으며 암염돔 측면 모형실험 결과 상부 수평층과 경사층 영상화가 적절하게 이루어졌음을 알 수 있었다. 특히 상부 수평층과 경사층이 하부층에 비해 뚜렸하게 나타나는 것은 이 부분에 탄성파 에너지가 집중되었음을 보여준다.
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- Publisher :The Korean Society of Mineral and Energy Resources Engineers
- Publisher(Ko) :한국자원공학회
- Journal Title :Journal of the Korean Society for Geosystem Engineering
- Journal Title(Ko) :한국지구시스템공학회지
- Volume : 42
- No :6
- Pages :625-633


Journal of the Korean Society of Mineral and Energy Resources Engineers







