The lower zone and the bronzite of the transition zone may be compared with the basal zone of the still-water complex. 下岩带和过渡带的古铜辉岩可与斯蒂尔沃特杂岩的基底岩带相比。
The intensity and falling area of the heavy storm could be reflected by the temperature advection intensity and the cold-warm transition belt location. 温度平流的强弱及冷暖过渡带位置能够较好地反映出降水的强度及落区。
