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- Cretaceous to Cenozoic 白垩纪-新生代
- From late Mesozoic era to Cenozoic era diwa tectonic evolution in the South China Sea may be divided into three stages: 1, From Late Cretaceous to Early Oligocene it was a stage of swelling and fracturing; 南海中生代末至新生代地洼构造演化分三个阶段:1,晚白垩世至早渐新世为属隆升破裂阶段;
- From the Cretaceous to the Early Cenozoic, it was uplifted again, until the Quaternary to build huge mountains with two large sedimentary basins on both sides. 从白垩纪到早新生代，它再度隆升，直至第四纪时形成雄伟的高大山系，两侧形成相应的大型沈积盆地。
- From late Cretaceous to Paleocene, it is the time of basin extruding, uplifting and denudation, therefore a larger angular unconformity formed between Mesozoic and Cenozoic. 到晚白垩世至古新世则为盆地挤压隆升剥蚀期，形成了中-新生界之间较大的角度不整合。
- The results show that the Cretaceous to Paleocene tectonic extension and compression alternated. 通过对不同地层单元断层滑动矢量的野外测量和古构造应力场反演，以及地层时代和同位素年代学测试结果的制约，建立了白垩纪-古新世构造应力场演替的年代序列。
- From Archeozoic to Cenozoic, there were magmatic actions in occurrence during every period. 从太古代到新生代,几乎各个时期都有岩浆活动。
- The durations of them are 230Ma, 203Ma, 221.4Ma and 145.6Ma respectively. The process from Cretaceous to Present passed only 3/4 of a complete cycle. 它们持续的时间分别为230，203，221?4，145?6Ma，其中白垩纪至今盆地演化过程大致经历了一个完整周期的3/4。
- The resumed subsidence history of the basin commendably reflects the evolution history of the basin from Late Cretaceous to Neogene. 本区沉积中心多表现为不对称的深凹区，沉积厚度巨大，是研究区生油层系的重要场昕。
- The upper structure layer is composed of the Cretaceous to the Quaternary, which shows a large slope dipping northwestward. 上构造层由白垩系-第四系构成，构造形态为-北西倾斜坡。
- We believe that there were platform sediments in the Paleozoic and the rifting depression sediments from Mesozoic to Cenozoic in the Yellow Sea area. 对南、北黄海沉积盆地形成的构造背景和盆地的构造类型进行了研究，认为在古生代它们是台地相沉积，中生代和新生代是张裂盆地；
- During extensional activities of Late Cretaceous to Eogene, intense upwelling of asthenosphere happened under the fault zone, leading to lithospheric necking in pure shear model. 断裂带在晚白垩世-早第三纪的伸展活动中,软流圈发生了强烈的上隆,岩石圈出现了显著的细颈化,属于纯剪切伸展模式。
- The Tan-Lu fault zone experienced intense extensional activities during the Late Cretaceous to the Early Paleogene.Thus, faulted basins were developed along the fault zone. 郯庐断裂带于晚白垩世至早第三纪经历了强烈的伸展活动，普遍控制发育了断陷盆地。
- A best chronology of the Cretaceous to Paleocene tectonic regimes has been established with the age constrained by stratigraphy and isotopic dating data. 这两个拆离系统分别形成于早白垩世莱阳群和晚白垩世-古新世王氏群沉积阶段。
- The Tan Lu fault zone turned into a huge extensional structure during Late Cretaceous to Eogene, leading to a series of development of fault bounded basins. 晚白垩世 早第三纪郯庐断裂带转变成巨型的伸展构造 ,普遍控制发育了断陷盆地。
- How much do all these figures stack up to? 这些数字的总和是多少？
- There was a long lag in forwarding mail to us. 转寄给我们的邮件晚了很久才拿到。
- Foreign nationals were asked to leave the country. 外国侨民被要求离开该国。
- A country must have the will to repel any invader. 一个国家得有决心击退任何入侵者。
- Swimming is the best way to tone up your body. 游泳是健体强身的最好方法。
- The Yongkang, Tiantai and Qujiang Groups are the synchronous heteropic accumulation during the late Early Cretaceous to the Late Cretaceous, and it is impossible for them to overlap each other. 永康群、天台群和衢江群是早白垩世晚期至晚白垩世时期的同期异相堆积，不存在相互叠覆关系。
