1) interior lake basin
内陆湖盆
1.
This paper describes the conditions of paleaogeography and paleaoclimate in triassic, and the development, accumulational and residual features of interior lake basins in late triassic epoch, besides these it also discusses the developed degree of tropical karst in middle and late triassic epoches in Guilin.
文章对桂林三叠世时的古地理及古气候条件、晚三叠世内陆湖盆的发育及堆积物和残留特征进行了描述,探讨了中晚三叠世桂林热带岩溶发育的程度。
2) lacustrine basin
陆相湖盆
1.
Sequence type and lithologic trap distribution in lacustrine basin of East China;
中国东部陆相湖盆层序类型与岩性圈闭发育特征
3) inland basin
内陆盆地
1.
Discuss on the representative enrichment mechanism of groundwater in the front of mountain around Inland Basin;
西北内陆盆地山前带典型地下水赋存模式探讨
2.
Study on the distribution and balance of the salt in the inland basin;
内陆盆地的盐分布与平衡分析研究
3.
Vertical water cycle and its ecological effect in inland basins, Northwest China;
中国西北内陆盆地水分垂直循环及其生态学意义
4) basin-making of continental interior
陆内造盆
5) intracontinental basin
陆内盆地
6) flows-in lake basin
内流湖盆
1.
The physical geography environment,the forming and distributing of the water resource in Ali area of Tibet are analyzed,basing on the difference of the groundwater resource forming environment,the water circulation system can be divided into alluvium and diluvium groundwater of rivervale in south and flows-in lake basin groundwater in north.
分析了西藏阿里地区自然地理环境、水资源形成和分布及其利用状况,基于区内地下水资源形成环境条件的差异,本区地下水资源体系可分为南部河谷冲洪积层地下水系统和北部内流湖盆地下水系统。
补充资料:湖盆
湖盆 lake basin 地表上汇集水体的相对封闭的洼地。形似盆状。湖盆成因有地壳运动形成的,如断陷湖盆、坳陷湖盆;还有外力作用形成的,如冰蚀湖盆、堆积湖盆等,此外也有人类经济活动形成的,如水库库区等。湖盆可以由5部分组成:湖岸、沿岸带、岸边浅滩、水下斜坡、湖盆底。湖泊面积的大小,湖盆地质条件和水流动态不同,湖盆的形态也有差异。研究湖盆的形态及其变化,有助于了解湖泊的起源、发展;湖泊的容积、湖水的理化性质和水文形势的变化。 |
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