模型将东亚大陆限定在一梯形边界框架之中,大陆岩石层被视为由幂指数律控制的薄层,它上伏在粘滞性较低的软流层之上蠕变流动。
In this model the EastAsia continent is limited in a trapezoid geological frame and the continental lithosphere is regard as a continuum thin plate with a power law rheology.
考虑到算法映射问题的NP复杂度和求解时间的指数性增加,本文主要研究两步规划方法,即先进行数据流图的最优规划,然后进行处理器的映射。
Because of the NP complexity of mapping problem, the thesis studies two-step method: optimal scheduling of data flow graph and optimal processor mapping.
考虑到算法映射问题的NP复杂度和求解时间的指数性增加,本文主要研究两步规划方法,即先进行数据流图的最优规划,然后进行处理器的映射。
Because of the NP complexity of mapping problem, the thesis studies two-step method: optimal scheduling of data flow graph and optimal processor mapping.
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