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1)  Cenozoic geography
新生代地理学
1.
Cenozoic geography is an important branch of physical geography, the aim of Cenozoic geography is to reconstruct the geographical environment change processes during Cenozoic Era, which help us to understand thedevelopment and evolution process of the physical geographical environment, so as to forecast its evolution trendin the future.
回顾了近40年来自然地理学的分支学科──新生代地理学的创立、发展历程,分析了该学科在强化地理学基础理论研究、拓宽应用研究以服务于国家社会经济建设的作用,揭示了新生代地理学研究与全球变化研究的密切联系及其未来发展的方向。
2)  palaeogeography of the Meso-Cenozoic
中新生代古地理
3)  New geography
新地理学
1.
We divide the development of French geography into three stages: the specialized stage, the New geography and the modern stage, and perform comments in briefly.
本文主要通过分析美国地理学、现代西方社会思潮和科技进步对法国地理学的影响,分专门化、新地理学和现代化三个阶段来阐述20世纪50年代以来其发展状况,并加以简要评述。
4)  Cenozoic basins
新生代盆地
1.
The initial forming time of Cenozoic basins in western Yunnan is at 14 Ma or so,it was coupling in the later period tectonic activity time of Lushui-Ruili arc dextral strike-slip fault belt in the eastern fringe and Nabang dextral strike-slip fault belt in the western fringe of Tengchong microplate.
滇西新生代盆地初始成盆时间约为14Ma,与腾冲微板块东缘泸水-瑞丽弧形右旋走滑断裂带和西缘那邦右旋走滑断裂带晚期活动时间相耦合。
2.
There contained abundant uranium resources in the Cenozoic basins, western Yunnan,where 8 small-sized or medium-sized sandstone-type uranium deposits have been prospected,and which is one of the important belts of sandstone-type uranium mineralization in China.
滇西新生代盆地内蕴藏着丰富的铀资源,现已探明8个中、小型砂岩型铀矿床,是中国重要的砂岩型铀矿成矿带之一。
5)  Cenozoic basin
新生代盆地
1.
Recgntion of Petroleum Exploration in the Cenozoic Basin of the East China Sea;
东海新生代盆地找油气的几点认识
2.
In the paper, we research mainly division of sub tectonic unit and the geological significance in Bohai offshore area, indicating the difference of petrology condition of different positive sub tectonic unit in Cenozoic basin and the necessary of right understanding and accurite division.
以渤海海域探区内二级构造单元的划分及其地质意义为重点 ,阐述了新生代盆地不同类型的二级正向构造单元在石油地质条件方面的差异性和正确认识和严格划分的必要性。
3.
All Cenozoic basinsin the east margin of Eurasia Plate have delimited by Y,Rand R’fractures .
欧亚板块东缘新生代盆地具有惊人相似的几何学特征,盆地边界均为Y 断裂及R,R’断裂,平面形态呈准菱形( 或Z形),均为右行剪切拉分盆地。
6)  Cenozoic Layer
新生代地层
1.
Heat Generation of the Cenozoic Layer of East China Sea Shelf;
我国东海陆架区新生代地层岩石生热率研究
补充资料:部门或专题军事地理学(见军事地理学)


部门或专题军事地理学(见军事地理学)
sectorial or thematic military geography

bumen huo zhuanti lunshi diliXue部门或专题军事地理学(sec‘orial orthematie military geography)见军事地理学。
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