其实上面这样的推算法，就是用所谓的递回推算 (solution by iteration)。我 们再回到用 (1.2) 式的符号来表示，可以得到一般化的结果如下: y t = (a 1 ) t-1 y 1 ( 1.3 ) 换句话说，如果某一时间序列的...
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At each iteration, a master direction is obtained by solving one direction finding subproblem which always possesses a solution, and an auxiliary direction is yielded by an explicit formula.
在每次迭代中，主方向是通过求解一个总有解的寻找方向子问题产生，而辅助方向是由一显式公式计算产生。
Guided by seismic data, we use logging data to invert lithological parameters and bed thickness exactly by successive iteration, hence solving the problem of multi solution in inversion.
即从测井数据出发，在地震资料的控制下，通过逐次迭代，精确地反演岩性及厚层参数，有效地解决了反演的多解性问题。
Then, the solution can be accurately solved by use of Newton Raphson Iteration.
然后，结合牛顿-拉夫森迭代法进行解的精确化。
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