Finally, we discuss and analyze the microcosmic mechanism of the characteristic of rock hysteresis briefly using P-M model.
最后对岩石滞回特性的微观机制用P - M模型作了简要讨论和分析。
However, the traditional M-P neuron model which used connective weights and a nonlinear activation function simulate the operation of neural's synapse and soma respectively.
然而，传统神经元的M - P模型用连接权值和非线性激活函数分别模仿神经元的突触和细胞体的作用。
The time signatures in the model move in six-hour increments from midnight (00:00 Universal time, or UTC) to 6 p. m. (18:00).
模型中的时间是从午夜(国际时间00：00，缩写utc)到下午6点(18：00)每六小时变化一次。
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