深圳(罗湖)-香港(元朗)断裂带的特征及其稳定性研究

The Characteristic and Stability Studies on Shenzhen(Luo Hu)-Hong Kong(Yuen Long) Fault Belt

本文尝试在编制深、港地质构造图的基础上，讨论区域主要构造体系演变史，概述断裂带的主要特征及其最新活动时期的证据，初步进行地震活动性及地震地质灾害的分析。

In the east of Guang Dong province,the NEE trending Lianhuashan abyssal fault consists of both east and west belts The west belt is named Wu Hua Shenzhen fault belt and the east belt named Dapu Hai Feng fault, is located in the southwest tip of the first fault belt A lot of engineering boring data demonstrate that Luo Hu Yuen fault is exposed in the bore boles on the right side of Shenzhen reservoir,then passes away in the south of Fu Tian Bonded Area and finally connects with Laufaushan Fauto in Hong Kong The main fault of Da Pu Hai Feng Fault trends morthcast from Tian Luo Kong area in Shenzhen,connccting with Mi Pu Fault in Hong Kong In the range of Luo Hu Yun Long fault belt, a lot of rock soil engineering projects have been accomplished, which make the seismic earthquake risk evaluation become a necessary task In coordination with seismic department,seismic safety analyses should be done and seismic desige parameters must be determined in major rock soil engineering projects,which will provide the important material for the seismic safety design of a building and the reliable basis for the disaster alleviation and facilities against earthquakes of the urban construction