结果表明：立水桥附近区域的浅部（150m以内）地层为3层结构，黄庄&高丽营断裂是由多条断层组合而成的、至今仍在活动的隐伏断裂；
The results indicate that there exists structure of three layers at the shallow part of the area , and the active fault consists of many concealed faults which remain active at present .
立水桥