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。
Maoduqing gold deposit occurred in the green schist and marble stratum transitional belt of paleoprotozoic Erdaowa Group in Inner Mongolia. 卯独庆金矿床赋存在古元古代二道凹岩群的绿片岩层与大理岩层过渡带。
