1.ON THE PIEDMONT SCARP IN DILUVIAL FAN OF Mt. HELANSHAN
初论贺兰山前洪积扇断层陡坎
2.It is feasible to infer the specific shape of a fault scarp with the help of its average diffusion age and origin time of the scarp.
无论是单一型断层崖还是复合型断层崖，通过断层崖的平均扩散年龄和初始错断时间，就能推断出它在某一时刻的具体形态。
3.The solution of the diffusion equation can be used to simulate the evolution of some kinds of scarp slopes.
摘要扩散方程可以用来模拟某些坡地演化形态。
4.The fault scarp in ground surface approximately is along the fault face that consists of Cretaceous sandstone and Archaean gneiss.
断层陡坎与白垩系砂岩和太古界片麻岩之间的断层位置大致吻合。
5.The government must listen to the voice of the people and immedaitely scarp the plan to build more towers in the state.
详细的时间和地点将会在每个星期三的报章上公布，敬请留意。
6.As the evolution process of the drainage channels on the scarp slope is concerned, the construction of their mathematic models and the visualization methods are discussed.
对断层崖上的沟谷演化过程，我们也对其数学模型的构造和可视化方法进行了探讨。
