撞击表明了前新生代盆地的结构，残余厚度和地下三分性。
Pre-Cenozoic basin structure, residual thickness and trichotomous property of basement are all shown by the impact.
辽宁省中新生代盆地地层中赋有有丰富的地热资源。
Rich geothermal resources are hosted in the Meso-Cenozoic basins in Liaoning Province.
潍北盆地是发育于郯庐断裂带内的中、新生代盆地。
Weibei basin is a Mesozoic-Cenozoic basin developed in the Tanlu fault zone.
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