2D多尺度非线性地震速度成像  

2D multiscale non-linear seismic velocity imaging

作　　者：潘纪顺[1,2] 张先康[1] Zhao Ping 徐朝繁[1] 刘志[1] 田晓峰[1] 殷智武 

机构地区：[1]中国地震局地球物理勘探中心,郑州450002 [2]中国地震局地球物理研究所,北京100081 [3]PGS Australia Pty Ltd, 1060 Hay St, West Perth, Western Australia, 6005 [4]辽宁有色勘察研究院,沈阳110013

出　　处：《地球物理学报》2008年第1期197-205,共9页Chinese Journal of Geophysics

基　　金：国家自然基金(40334040和40474049)项目资助

摘　　要：将遗传算法和单纯形算法相结合,得到了一种高效、健全的2D混合地震走时反演方法.把速度场划分为不同的空间尺度,定义网格节点上的速度作为待反演参数,采用双三次样条函数模型参数化,正问题采用有限差分走时计算方法,反问题采用多尺度混合反演方法.首先在较大的空间尺度内反演,然后减小空间尺度,将大尺度的反演结果作为次一级尺度反问题的初始模型,再进行混合反演,如此类推逐次逼近全局最优解.一个低速度异常体的数值模拟试验和抗走时扰动试验表明该方法是有效和健全的.我们将该方法应用到青藏高原东北缘阿尼玛卿缝合带东段上部地壳速度结构研究中,并与前人的成果进行了对比.A hybrid algorithm of the global genetic algorithm （GA） and the local simplex method are proposed to form an efficient and robust 2D muhi-scale non-linear seismic travehime inversion method. The background velocity field is estimated at a spatially varying grid. The velocities at the nodes of the grid are regarded as inversion parameters. The model is parameterized by a bicubic spline function. The forward problem is calculated by use of the finite-difference method. The inverse problem is solved by the muhiscale hybrid inverse method . First, the inversion is done in large spatial scale, and then take its results as the initial value for inversion in next spatial scale. The inversion result will be closer to the global optimization. The method was tested to be efficient and robust by numerical simulating. An anomalous velocity area in the test model could be reconstructed and the result is stable when adding random noise to travehimes. We also used the method to research the upper crustal structure features of A＇nye^^maqe^^n suture zone. At last, we compared our research results with that obtained by use of other method.

关 键 词：多尺度 地震走时 非线性 反演 阿尼玛卿缝合带 

分 类 号：P315[天文地球—地震学]