Abstract:Through analyzing physical geography, geology and hydrogeology condition, combining with characteristics of distribution, occurrence and movement of groundwaterbearing layers, and influence of geological structures on karst development and groundwater movement, it is concluded that groundwater is relative enrichment at tectonic fracture zone of runoff replenishment areas. Characteristics of groundwater enrichment can be divided into structural belt controlling type, igneous bodies barrier richwater type, faults influencing abundant water type and away fracture zone weakenrichment water type. Through study and analysis on groundwater enrichment rules of groundwater recharge to groundwater runoff, it will provide some references for borehole location in water shortage mountain areas.