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1)  Lanping Mesozoic Cenozoic Basin
兰坪中新生代盆地
2)  Lanping Basin
兰坪盆地
1.
Fluid dynamic processes of large-scale mineralization in the Lanping Basin,Yunnan,SW-China:evidence from fluid inclusions and basin fluid modeling;
西南三江兰坪盆地大规模成矿的流体动力学过程——流体包裹体和盆地流体模拟证据
2.
A Discussion on the Helium and Argon Isotopic Evidences for Genesis of the Baiyangping Copper—Cobalt Deposit in the Lanping Basin;
论兰坪盆地白秧坪铜(钴)矿床成因的氦氩同位素证据
3.
THE SYNTHETIC ANALYSIS OF REMOTE SENSING AND GEO-ANOMALY ON ORE-FORMING PREDICTION--Taking the Lanping basin as an example;
成矿预测中遥感与地质异常的综合分析——以兰坪盆地为例
3)  Meso-Cenozoic basin
中新生代盆地
1.
Tectonics and deep structure features of Meso-Cenozoic basin groups,northern NE China;
东北北部中新生代盆地群构造与深部结构特征
2.
The tectonic-thermoregime of lithosphere and Meso-Cenozoic basin in Mainland China.;
中国大陆岩石圈与中新生代盆地构造-热体制
3.
Rich geothermal resources are hosted in the Meso-Cenozoic basin s in Liaoning Province.
辽宁省中新生代盆地地层中赋有有丰富的地热资源。
4)  Mesozoic and Cenozoic basins
中、新生代盆地
5)  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。
6)  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。
补充资料:中中新世山旺盆地生态复原图




中中新世山旺盆地生态复原图  
                                       赵野木绘
  [图]图

说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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