1) neogenic structure
新生构造
1.
According to the orientations,the younger structures can be classified into two basic kinds: inherited and neogenic structures.
中国及邻区大陆是经多期造山运动形成的复合大陆,后期构造可分为继承性构造和新生构造两种。
2.
The paper discussed,in succession of tectonic cycles,the neogenic structures in each part,including the ages,orientations and active modes.
分阶段讨论了塔南、塔中和塔北地区各期新生构造的形成时代、方向和活动方式,并从与周缘造山带耦合演化的角度探讨了其形成机制,分析了其海相油气勘探意义。
3.
The roles of controlling basin development of the fractures with varied strikes,including the W-E and NE-striking fractures in the basement,were analysed,which emphasized that the neogenic structures of N-S orientation appearing in Mesoproterozoic and NW-striking forming in Early Ordovician played an important part in the fault-block\'s evolution and oil-gas accumulation.
分析了不同方向的断裂(包括基底中的东西向和北东向断裂)在盆地发育中所起的作用,强调了中元古代出现的南北向新生构造和早奥陶世出现的北西向新生构造在断块演化和油气成藏中的重要性,并以"盆""山"耦合发育为指导探讨了这两者及东西向断裂与邻侧造山带演化间的有机联系。
3) Late Cenozoic tectonic movement
晚新生代构造
1.
Late Cenozoic tectonic movement in the Keyir Mountain area,Kuqa,Xinjiang,and its controls on sandstone-type uranium deposits;
新疆库车黑英山地区晚新生代构造运动及其对砂岩型铀矿成矿的控制作用初析
4) Cenozoic tectonic uplift
新生代构造抬升
1.
The global Cenozoic tectonic uplift, especially the uplift of Himalayan mountain beltTibet plateau in southern Asia,Andean mountain and Altiplano plateau in southern America, have the strong effects on the Earth surface chemical weathering and global climate change.
全球新生代构造抬升 ,特别是南亚喜马拉雅青藏高原和南美安底斯山脉和Altiplano高原在新生代的抬升对地表化学风化和全球气候变化产生了重要影响。
5) NW-striking neogenic structure
北西向新生构造
6) NE-trending neogenic structure
北东向新生构造
补充资料：《新生》事件
见《新生》。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条