遂昌柘岱口—湖山北东向断裂带在晚侏罗世至晚白垩世晚期经历了多期次、不同性质的活动，断裂活动与该地区两个大规模萤石矿田的形成关系密切。
Zhedaikou-Hushan north-east strike fracture zone with several active stages possessed the characteristics of inherited basal structure from late stage of late Jurassic to late Cretaceous.
通过野外地质调查并结合前人资料，对蒙甘青地区白垩纪原型盆地沉积特征及盆山格局进行了研究。
Depositional setting and basin-mountain framework of Cretaceous proto-basin of Iner Mongolia-Gansu-Qinghai area is reconstructed based on field geological survey and previous works of others.
白垩纪造山活动再次加强，盆地处于第二个发育期。
In Cretaceous, while the orogenic activity strengthened once more, the basin was in the second developing period.
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