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目前,国内外城市地质研究正方兴未艾。深圳市区域稳定性评价是城市地质研究新开辟的领域,是地震工作者值得关注的新动向。 深圳市位于五华—深圳断裂带的南段。高楼林立的罗湖区正好建筑在这条断裂带上。因而引起了国内外人士的关注。严峻的问题摆在地学工作者面前:深圳的地基地质是否稳定?能否继续进行城市建设? 为了探讨这个问题,1984年地矿部决定投资170余万元,由水文地质工程地质司组织地
At present, the research on urban geology at home and abroad is in the ascendant. The evaluation of regional stability in Shenzhen City is a newly opened area of urban geology research and a new trend that earthquake workers deserve our attention. Shenzhen is located in the southern part of Wuhua-Shenzhen fault zone. High-rise buildings in Luohu District just built on this fault zone. Which has aroused the concern of people at home and abroad. In front of the geoscientists: the foundation of Shenzhen is stable? Can continue to carry out urban construction? In order to explore this issue, in 1984 the Ministry of Mines decided to invest 170 million yuan, organized by the Department of Hydrogeology and Engineering Geology