云南地区速度结构的横向不均匀性

本文利用了地震层析技术的原理和方法,在云南地区成功地重建了10个不同深度的速度剖面图象,这些速度剖面和6条深地震测深的速度剖面一致。本文使用的重建方法有两大优点:(1) 速度模式是通过指定节点速度和通过已知基函数的线性插值而确定,这样就建立了一个横向连续而垂向不连续的速度场;(2) 速度参数和震源参数通过正交投影算子使之分离,采用顺序正交三角化和修正的奇异值分解,这些措施使内存的需要量减小一个量级,计算量减少一半。     

THE LATERAL INHOMOGENEITY IN YUNNAN PROVINCE, CHINA

Images of the velocity cross--section at 10 different depths in Yunnan Province have been suc-cessfully reconstructed, using the principle and method of seismic tomography (ST). These velocitycoss-sections are consistent with the results of six velocity profiles of deep seismic sounding. The reconstruction method of ST used in this paper has two advantages: (i) The velocity modeli determined by spe cifying node--velocities of hexahedron and linear interpolation through knownbasic function. A velocity field with lateral continuous velocity value and vertical discontinuitiesis established. This model is obviously better than the block model of constant velocity. The verticaldiscontinuities allow the model to simulate velocity discontinuities in the crust and upper mantle. (ii)The velocity and hypocenter parameters are separated by introducing an orthogonal projection oper-ator. Sequential orthogonal triangularization and modified singular decomposition are adopted.These measures reduce the RAM requirement