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.
六盘山白垩纪盆地是六盘山内陆叠合盆地的一个单型盆地。
Liupanshan Cretaceous basin is a mono-basin of Liupanshan inland overlapping basin.
六盘山盆地位于河西走廊东南端，处于鄂尔多斯盆地西缘，白垩纪是其主要成盆期。
The Liupanshan Basin. which was mainly formed during the Cretaceous. is located in the southeastern tip of the Hexi Corridor and on the west of the Ordos Basin.
大别造山带北部的北淮阳中生代火山喷发岩带形成于后造山阶段的晚侏罗世—早白垩世。
Mesozoic volcanic eruption belt, which locates on Beihuaiyang area in northern part of Dabie orogenic belt, formed at post orogenic stage during Late Jurassic to Early Cretaceous.
现代地质学研究表明，雁荡山是一座具有世界意义的典型的白垩纪流纹质古火山——破火山。
Modern geology studies have shown that Hill is a world with a sense of typical Cretaceous rhyolitic ancient volcano - caldera.
磷灰石裂变径迹研究表明，六盘山盆地白垩系地层经历两次埋深加热事件。
Apatite fission track data suggest that the early Cretaceous strata in the Liupanshan basin were subjected to two burial heating events.
磷灰石裂变径迹研究表明，六盘山盆地白垩系地层经历两次埋深加热事件。
Apatite fission track data suggest that the early Cretaceous strata in the Liupanshan basin were subjected to two burial heating events.
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