It was considered that method of equilibriumprofile is the best method to recognize and quantitatively study active thrust fault and underlying fault.
而平衡剖面法乃是识别和定量研究活动逆断层，特别是隐伏断层的最好方法。
2
In condition of uniform stratum and unchanged flow, the process of equilibriumprofile forming is similar to a mathematic question-Toboggan slide with the least time.
均质地层和定流量条件下均衡纵剖面的形成过程与最速滑降问题类似。
3
The equilibrium beach profile is a statistically relative equilibrium beach shape under the interaction between Marine dynamics and beach sediments.