Abstract:A method for igneous rock velocity-depth model building is put forward in this paper. According to the special geological features of igneous rocks, we extract accurately the low frequency component of seismic imaging velocity from VSP and other priori information. Then we optimize velocity-depth model with three-dimensional grid tomography to obtain the high-frequency component of seismic imaging velocity. This method reduces the influence of multiple solutions in the process of velocity inversion, and then igneous rocks can be more accurately imaged. Application results on real data show that the proposed method can well image not only igneous rocks but also overlying strata under igneous rocks.
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