论文部分内容阅读
密山市地形地貌与地质构造控制了密山市地下水的形成和运动规律在低山丘陵区形成风化裂隙水,在山前台地形成裂隙孔隙潜水,在平原区形成孔隙潜水。
The formation and movement of groundwater in Mishan City are controlled by the topography and geological structure in Mishan City. Formation of weathered fissure water in the hilly area, formation of fissured pore water in the mountain front and formation of pore diving in the plain area.