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莱芜县位于鲁中山区中部,总面积为540平方公里,地貌为一构造断陷盆地。受区域地质构造控制,下古生界石灰岩地层主要分布在盆地南部的低山丘陵,盆地东部、北部的边缘山区有零星出露,石灰岩区经历多次地质构造运动,受多种构造体系的干扰,断层、裂隙发育,水动力条件复杂,是我县找水工作重点。十几年来,我们运用地
Laiwu County is located in the central Lushan Mountain, with a total area of 540 square kilometers, the topography of a structural fault basin. Under the control of the regional geological structure, the Lower Paleozoic limestone formations are mainly distributed in the hilly hills in the south of the basin. Sporadic outcrops occur in the marginal mountainous areas in the eastern and northern parts of the basin. The limestone area undergoes several geological tectonic movements and is disturbed by various tectonic systems , Faults, fissures development, hydrodynamic conditions are complex, is the focus of my county to find water. Ten years, we use the ground