1) Wenshan Basin
文山盆地
1.
The Engineering Geologic Subdivision of Wenshan Basin and the Evaluation on the Suitability of the Land Use for Urban Construction;
文山盆地工程地质分区及城市建设用地适宜性评价
2.
Based on geo-environment in Wenshan basin,setting out from the factors of topography、the geotechnical character、environmental hydrology geotechnical character、geological hazards and construction to appraise feasibility evaluation between city geological environment and urban development.
本文从文山盆地基础地质环境条件出发,以地形地貌、岩土工程地质条件、环境水文地质条件、地质灾害和构造条件等影响地质环境质量的主要因素入手,最终对城市地质环境与城市发展的适宜性进行评价。
2) Baoshan Basin
保山盆地
1.
Evaluation of geochemical characteristics of hydrocarbon source rock and gas-generating potential in Upper Tertiary, Baoshan Basin;
保山盆地上第三系烃源岩地化特征及气源潜力评价
2.
Time-space distribution of the sands in the third member of Yangyi formation,Yongzhujie uplift,Baoshan Basin;
保山盆地永铸街凸起羊邑组三段砂体时空展布规律研究
3.
Biological Gas Resource and its Exploration Potential in Neogene,Baoshan Basin;
保山盆地新近系生物气资源及勘探前景
3) Xiangshan basin
相山盆地
1.
The distributing character of the magnetic structure was inverse at the different depth of Xiangshan basin.
相山矿田是我国最主要的铀矿资源基地之一,本文介绍了综合利用位、场及场的垂直梯度的物性反演方法的原理与实施,反演计算了相山盆地不同深度下的磁性结构分布特征,最后对相山盆地地下岩层结构及界面变化趋势进行了半定量和定性分析,这对指导相山的铀资源勘查有着重要意义。
4) volcanic basin
火山盆地
1.
Strike-slip pull-apart process and emplacement of Xiangshan uranium-producing volcanic basin;
走滑拉分作用与相山产铀火山盆地的就位
2.
Geological conditions for ore-forming process and prospecting direction of the U-Mo polymetallic deposits in Guyuan volcanic basin;
沽源火山盆地铀钼多金属成矿地质条件分析及找矿方向
3.
Lingquan volcanic basin is located in the mid-southern segment of known Rrguna-Kelulun Eastnorth-trending volcanic rocks uranium metallogenic belt,it is on the same belt with Telechuf Field of Russia and Durnuot Field of Mongolia.
灵泉火山盆地位于著名的额尔古纳—克鲁伦北东向火山岩铀成矿带中南段,与俄罗斯斯特列措夫铀矿田、蒙古多尔诺特铀矿田处于同一矿带上。
5) intermountain basin
山间盆地
1.
Located in a tectonic uplift region in Zixi county, Jiangxi province, the Fashui hot spring along the Erkou Shixia fault belt is a typical intermountain basin type hot spring with a geothermal anormaly area less than 1km 2.
构造上 ,它处在耳口 -石峡断裂带上的资溪背斜与嵩市向斜之间 ,产于隆起区山间盆地。
6) Mountain-basin
山系-盆地
补充资料：中中新世山旺盆地生态复原图
赵野木绘
[图]
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