| 甘肃西部北山区断裂构造对地下水的控制作用 |
| |
| 引用本文： | 尹政,赵艳娜,杨丽萍.甘肃西部北山区断裂构造对地下水的控制作用[J].地下水,2010,32(3):12-14,98. |
| |
| 作者姓名： | 尹政 赵艳娜 杨丽萍 |
| |
| 作者单位： | 甘肃省地矿局水文地质工程地质勘察院,甘肃,张掖,734000 |
| |
| 基金项目： | 甘肃省地矿局2009年地质勘查项目 |
| |
| 摘 要： | 甘肃西部北山区经历了多期构造运动,水文地质条件异常复杂,断裂构造严格控制着区内地下水的分布、埋藏及运动规律,主干断裂带与支干断裂的交汇部位、沟谷与断裂交汇带、新构造运动形成的沉降带及坳陷盆地等有利于地下水的赋存,可作为供水水源地水文地质勘探靶区。
|
| 关 键 词： | 断裂构造 地下水 控制 |
Control Function of the Break Structure for Groundwater in the North Mountain Area of the West Gansu Province |
| |
| YIN Zheng,ZHAO Yan-na,YANG Li-ping.Control Function of the Break Structure for Groundwater in the North Mountain Area of the West Gansu Province[J].Groundwater,2010,32(3):12-14,98. |
| |
| Authors: | YIN Zheng ZHAO Yan-na YANG Li-ping |
| |
| Institution: | 1.Institute of Hydrogeoloical and Engineering Geology,Gansu Provincial Bureau of Geology and Mineral Exploratation and Development,Zhangye 734000,Gansu;2.Geology Engineering Institute of Gansu Province,Zhangye 734000,Gansu) |
| |
| Abstract: | In the north mountain area of the west Gansu,there is experienced many tectogenesis.The hydrogeololgy condition is extraordinarily complicated.The break structure strictly control the groundwater distribution、the hidden or movement regulation in the area.The converge place which is the main and less important break,the exchanged area between the gully and the break,the subsided zone caused by the new structure movement and the sunken basin are benefit of groundwater enrichment,which is the target area of hydrogeology investigation for water-supplying source. |
| |
| Keywords: | The break structure Groundwater to Control and North mountain area |
| 本文献已被 维普 万方数据 等数据库收录！ |
|
