强制性水退机制作用下形成的砂体大都沉积在沉积滨线坡折带以下的齐家—古龙凹陷内，并逐渐向盆地方向进积迁移。
The sand bodies formed under the mechanism of forced regression are mostly deposited in Qijia-Gulong depression, and they prograde towards the basin gradually.
后滨沙丘蚀退、滩肩蚀低、岸线向陆迁移是地貌响应的主要特征；
The backshore dunes' retreating, the berms' lowering, and the shoreline's moving landwards was the main response feature of the profiles.
而我们的滨水中央公园作为一个独特的地标，向每一位抵达铜仁的访客展示一个极具吸引力的城市。
And waterfront central park as a unique landmark, for to every visitor shows an attractive city.
应用推荐