香港—九龙地区,中生代以来地壳发生了方向不同的水平挤压活动,多层席状地质层体相互叠覆。末次自北往南的推覆活动使北部地体拼贴、叠置在南部相对原地体上。各期推覆形迹叠加改造,构造形态殊异,地壳表部的断裂也都受制於这一机制。 Hong Kong - Kowloon area, the crust occurred in the direction of the different horizontal extrusion activities since the Mesozoic, multi-layered seat-like geological layers overlap each other. The last push from north to south caused the collapsing of the northern bodies to be superimposed on the southern relative to the original terrain. Various stages of nappe superimposed and remodeled, the tectonic forms of different, crustal surface of the fault are subject to this mechanism.